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пододделот Состав</span> </button> <ul id="toc-Состав-sublist" class="vector-toc-list"> <li id="toc-Геохемија" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Геохемија"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.1</span> <span>Геохемија</span> </div> </a> <ul id="toc-Геохемија-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Животен_циклус" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Животен_циклус"> <div class="vector-toc-text"> <span class="vector-toc-numb">1.2</span> <span>Животен циклус</span> </div> </a> <ul id="toc-Животен_циклус-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Магнетни_аномалии" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Магнетни_аномалии"> <div class="vector-toc-text"> <span class="vector-toc-numb">2</span> <span>Магнетни аномалии</span> </div> </a> <ul id="toc-Магнетни_аномалии-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Наводи" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Наводи"> <div class="vector-toc-text"> <span class="vector-toc-numb">3</span> <span>Наводи</span> </div> </a> <ul id="toc-Наводи-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Надворешни_врски" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Надворешни_врски"> <div class="vector-toc-text"> <span class="vector-toc-numb">4</span> <span>Надворешни врски</span> </div> </a> <ul id="toc-Надворешни_врски-sublist" class="vector-toc-list"> </ul> </li> </ul> </div> </div> </nav> </div> </div> <div class="mw-content-container"> <main id="content" class="mw-body"> <header class="mw-body-header vector-page-titlebar"> <nav aria-label="Содржина" class="vector-toc-landmark"> <div id="vector-page-titlebar-toc" class="vector-dropdown vector-page-titlebar-toc vector-button-flush-left" > <input type="checkbox" id="vector-page-titlebar-toc-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-page-titlebar-toc" class="vector-dropdown-checkbox " aria-label="Прик./скр. содржина" > <label id="vector-page-titlebar-toc-label" for="vector-page-titlebar-toc-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--icon-only " aria-hidden="true" ><span class="vector-icon mw-ui-icon-listBullet mw-ui-icon-wikimedia-listBullet"></span> <span class="vector-dropdown-label-text">Прик./скр. содржина</span> </label> <div class="vector-dropdown-content"> <div id="vector-page-titlebar-toc-unpinned-container" class="vector-unpinned-container"> </div> </div> </div> </nav> <h1 id="firstHeading" class="firstHeading mw-first-heading"><span class="mw-page-title-main">Океанска кора</span></h1> <div id="p-lang-btn" class="vector-dropdown mw-portlet mw-portlet-lang" > <input type="checkbox" id="p-lang-btn-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-p-lang-btn" class="vector-dropdown-checkbox mw-interlanguage-selector" aria-label="Појдете на статија на друг јазик. Достапно на 45 јазици" > <label id="p-lang-btn-label" for="p-lang-btn-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet cdx-button--action-progressive mw-portlet-lang-heading-45" aria-hidden="true" ><span class="vector-icon mw-ui-icon-language-progressive mw-ui-icon-wikimedia-language-progressive"></span> <span class="vector-dropdown-label-text">45 јазици</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D9%82%D8%B4%D8%B1%D8%A9_%D9%85%D8%AD%D9%8A%D8%B7%D9%8A%D8%A9" title="قشرة محيطية — арапски" lang="ar" hreflang="ar" data-title="قشرة محيطية" data-language-autonym="العربية" data-language-local-name="арапски" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Okean_yer_qab%C4%B1%C4%9F%C4%B1" title="Okean yer qabığı — азербејџански" lang="az" hreflang="az" data-title="Okean yer qabığı" data-language-autonym="Azərbaycanca" data-language-local-name="азербејџански" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-bh mw-list-item"><a href="https://bh.wikipedia.org/wiki/%E0%A4%B8%E0%A4%AE%E0%A5%81%E0%A4%82%E0%A4%A6%E0%A5%8D%E0%A4%B0%E0%A5%80_%E0%A4%95%E0%A5%8D%E0%A4%B0%E0%A4%B8%E0%A5%8D%E0%A4%9F" title="समुंद्री क्रस्ट — Bhojpuri" lang="bh" hreflang="bh" data-title="समुंद्री क्रस्ट" data-language-autonym="भोजपुरी" data-language-local-name="Bhojpuri" class="interlanguage-link-target"><span>भोजपुरी</span></a></li><li class="interlanguage-link interwiki-bg mw-list-item"><a href="https://bg.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанска кора — бугарски" lang="bg" hreflang="bg" data-title="Океанска кора" data-language-autonym="Български" data-language-local-name="бугарски" class="interlanguage-link-target"><span>Български</span></a></li><li class="interlanguage-link interwiki-ca mw-list-item"><a href="https://ca.wikipedia.org/wiki/Escor%C3%A7a_oce%C3%A0nica" title="Escorça oceànica — каталонски" lang="ca" hreflang="ca" data-title="Escorça oceànica" data-language-autonym="Català" data-language-local-name="каталонски" class="interlanguage-link-target"><span>Català</span></a></li><li class="interlanguage-link interwiki-cs mw-list-item"><a href="https://cs.wikipedia.org/wiki/Oce%C3%A1nsk%C3%A1_k%C5%AFra" title="Oceánská kůra — чешки" lang="cs" hreflang="cs" data-title="Oceánská kůra" data-language-autonym="Čeština" data-language-local-name="чешки" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-da mw-list-item"><a href="https://da.wikipedia.org/wiki/Oceanbundsplade" title="Oceanbundsplade — дански" lang="da" hreflang="da" data-title="Oceanbundsplade" data-language-autonym="Dansk" data-language-local-name="дански" class="interlanguage-link-target"><span>Dansk</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Ozeanische_Erdkruste" title="Ozeanische Erdkruste — германски" lang="de" hreflang="de" data-title="Ozeanische Erdkruste" data-language-autonym="Deutsch" data-language-local-name="германски" class="interlanguage-link-target"><span>Deutsch</span></a></li><li class="interlanguage-link interwiki-et mw-list-item"><a href="https://et.wikipedia.org/wiki/Ookeaniline_maakoor" title="Ookeaniline maakoor — естонски" lang="et" hreflang="et" data-title="Ookeaniline maakoor" data-language-autonym="Eesti" data-language-local-name="естонски" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-en mw-list-item"><a href="https://en.wikipedia.org/wiki/Oceanic_crust" title="Oceanic crust — англиски" lang="en" hreflang="en" data-title="Oceanic crust" data-language-autonym="English" data-language-local-name="англиски" class="interlanguage-link-target"><span>English</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/Corteza_oce%C3%A1nica" title="Corteza oceánica — шпански" lang="es" hreflang="es" data-title="Corteza oceánica" data-language-autonym="Español" data-language-local-name="шпански" class="interlanguage-link-target"><span>Español</span></a></li><li class="interlanguage-link interwiki-eo mw-list-item"><a href="https://eo.wikipedia.org/wiki/Oceankrusto" title="Oceankrusto — есперанто" lang="eo" hreflang="eo" data-title="Oceankrusto" data-language-autonym="Esperanto" data-language-local-name="есперанто" class="interlanguage-link-target"><span>Esperanto</span></a></li><li class="interlanguage-link interwiki-eu mw-list-item"><a href="https://eu.wikipedia.org/wiki/Lurrazal_ozeaniko" title="Lurrazal ozeaniko — баскиски" lang="eu" hreflang="eu" data-title="Lurrazal ozeaniko" data-language-autonym="Euskara" data-language-local-name="баскиски" class="interlanguage-link-target"><span>Euskara</span></a></li><li class="interlanguage-link interwiki-fa mw-list-item"><a href="https://fa.wikipedia.org/wiki/%D9%BE%D9%88%D8%B3%D8%AA%D9%87_%D8%A7%D9%82%DB%8C%D8%A7%D9%86%D9%88%D8%B3%DB%8C" title="پوسته اقیانوسی — персиски" lang="fa" hreflang="fa" data-title="پوسته اقیانوسی" data-language-autonym="فارسی" data-language-local-name="персиски" class="interlanguage-link-target"><span>فارسی</span></a></li><li class="interlanguage-link interwiki-fr mw-list-item"><a href="https://fr.wikipedia.org/wiki/Lithosph%C3%A8re_oc%C3%A9anique" title="Lithosphère océanique — француски" lang="fr" hreflang="fr" data-title="Lithosphère océanique" data-language-autonym="Français" data-language-local-name="француски" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-ga mw-list-item"><a href="https://ga.wikipedia.org/wiki/Screamh_aig%C3%A9anach" title="Screamh aigéanach — ирски" lang="ga" hreflang="ga" data-title="Screamh aigéanach" data-language-autonym="Gaeilge" data-language-local-name="ирски" class="interlanguage-link-target"><span>Gaeilge</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/Codia_oce%C3%A1nica" title="Codia oceánica — галициски" lang="gl" hreflang="gl" data-title="Codia oceánica" data-language-autonym="Galego" data-language-local-name="галициски" class="interlanguage-link-target"><span>Galego</span></a></li><li class="interlanguage-link interwiki-ko mw-list-item"><a href="https://ko.wikipedia.org/wiki/%ED%95%B4%EC%96%91_%EC%A7%80%EA%B0%81" title="해양 지각 — корејски" lang="ko" hreflang="ko" data-title="해양 지각" data-language-autonym="한국어" data-language-local-name="корејски" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-hi mw-list-item"><a href="https://hi.wikipedia.org/wiki/%E0%A4%AE%E0%A4%B9%E0%A4%BE%E0%A4%B8%E0%A4%BE%E0%A4%97%E0%A4%B0%E0%A5%80%E0%A4%AF_%E0%A4%AD%E0%A5%82%E0%A4%AA%E0%A4%B0%E0%A5%8D%E0%A4%AA%E0%A4%9F%E0%A5%80" title="महासागरीय भूपर्पटी — хинди" lang="hi" hreflang="hi" data-title="महासागरीय भूपर्पटी" data-language-autonym="हिन्दी" data-language-local-name="хинди" class="interlanguage-link-target"><span>हिन्दी</span></a></li><li class="interlanguage-link interwiki-hr mw-list-item"><a href="https://hr.wikipedia.org/wiki/Oceanska_kora" title="Oceanska kora — хрватски" lang="hr" hreflang="hr" data-title="Oceanska kora" data-language-autonym="Hrvatski" data-language-local-name="хрватски" class="interlanguage-link-target"><span>Hrvatski</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Kerak_samudra" title="Kerak samudra — индонезиски" lang="id" hreflang="id" data-title="Kerak samudra" data-language-autonym="Bahasa Indonesia" data-language-local-name="индонезиски" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-is mw-list-item"><a href="https://is.wikipedia.org/wiki/Hafsbotnsskorpa" title="Hafsbotnsskorpa — исландски" lang="is" hreflang="is" data-title="Hafsbotnsskorpa" data-language-autonym="Íslenska" data-language-local-name="исландски" class="interlanguage-link-target"><span>Íslenska</span></a></li><li class="interlanguage-link interwiki-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Crosta_oceanica" title="Crosta oceanica — италијански" lang="it" hreflang="it" data-title="Crosta oceanica" data-language-autonym="Italiano" data-language-local-name="италијански" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-ky mw-list-item"><a href="https://ky.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD_%D1%82%D0%B0%D0%BC%D0%B0%D0%BD%D1%8B" title="Океан таманы — киргиски" lang="ky" hreflang="ky" data-title="Океан таманы" data-language-autonym="Кыргызча" data-language-local-name="киргиски" class="interlanguage-link-target"><span>Кыргызча</span></a></li><li class="interlanguage-link interwiki-lv mw-list-item"><a href="https://lv.wikipedia.org/wiki/Oke%C4%81nisk%C4%81_Zemes_garoza" title="Okeāniskā Zemes garoza — латвиски" lang="lv" hreflang="lv" data-title="Okeāniskā Zemes garoza" data-language-autonym="Latviešu" data-language-local-name="латвиски" class="interlanguage-link-target"><span>Latviešu</span></a></li><li class="interlanguage-link interwiki-ms mw-list-item"><a href="https://ms.wikipedia.org/wiki/Kerak_lautan" title="Kerak lautan — малајски" lang="ms" hreflang="ms" data-title="Kerak lautan" data-language-autonym="Bahasa Melayu" data-language-local-name="малајски" class="interlanguage-link-target"><span>Bahasa Melayu</span></a></li><li class="interlanguage-link interwiki-nl mw-list-item"><a href="https://nl.wikipedia.org/wiki/Oceanische_lithosfeer" title="Oceanische lithosfeer — холандски" lang="nl" hreflang="nl" data-title="Oceanische lithosfeer" data-language-autonym="Nederlands" data-language-local-name="холандски" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-ja badge-Q70894304 mw-list-item" title=""><a href="https://ja.wikipedia.org/wiki/%E6%B5%B7%E6%B4%8B%E6%80%A7%E5%9C%B0%E6%AE%BB" title="海洋性地殻 — јапонски" lang="ja" hreflang="ja" data-title="海洋性地殻" data-language-autonym="日本語" data-language-local-name="јапонски" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-no mw-list-item"><a href="https://no.wikipedia.org/wiki/Havbunnsskorpe" title="Havbunnsskorpe — норвешки букмол" lang="nb" hreflang="nb" data-title="Havbunnsskorpe" data-language-autonym="Norsk bokmål" data-language-local-name="норвешки букмол" class="interlanguage-link-target"><span>Norsk bokmål</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/Havbotnskorpe" title="Havbotnskorpe — норвешки нинорск" lang="nn" hreflang="nn" data-title="Havbotnskorpe" data-language-autonym="Norsk nynorsk" data-language-local-name="норвешки нинорск" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Skorupa_ziemska_oceaniczna" title="Skorupa ziemska oceaniczna — полски" lang="pl" hreflang="pl" data-title="Skorupa ziemska oceaniczna" data-language-autonym="Polski" data-language-local-name="полски" class="interlanguage-link-target"><span>Polski</span></a></li><li class="interlanguage-link interwiki-pt mw-list-item"><a href="https://pt.wikipedia.org/wiki/Crusta_oce%C3%A2nica" title="Crusta oceânica — португалски" lang="pt" hreflang="pt" data-title="Crusta oceânica" data-language-autonym="Português" data-language-local-name="португалски" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D0%B8%D1%87%D0%B5%D1%81%D0%BA%D0%B0%D1%8F_%D0%BA%D0%BE%D1%80%D0%B0" title="Океаническая кора — руски" lang="ru" hreflang="ru" data-title="Океаническая кора" data-language-autonym="Русский" data-language-local-name="руски" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-simple mw-list-item"><a href="https://simple.wikipedia.org/wiki/Oceanic_crust" title="Oceanic crust — Simple English" lang="en-simple" hreflang="en-simple" data-title="Oceanic crust" data-language-autonym="Simple English" data-language-local-name="Simple English" class="interlanguage-link-target"><span>Simple English</span></a></li><li class="interlanguage-link interwiki-sk mw-list-item"><a href="https://sk.wikipedia.org/wiki/Oce%C3%A1nska_zemsk%C3%A1_k%C3%B4ra" title="Oceánska zemská kôra — словачки" lang="sk" hreflang="sk" data-title="Oceánska zemská kôra" data-language-autonym="Slovenčina" data-language-local-name="словачки" class="interlanguage-link-target"><span>Slovenčina</span></a></li><li class="interlanguage-link interwiki-sl mw-list-item"><a href="https://sl.wikipedia.org/wiki/Oceanska_skorja" title="Oceanska skorja — словенечки" lang="sl" hreflang="sl" data-title="Oceanska skorja" data-language-autonym="Slovenščina" data-language-local-name="словенечки" class="interlanguage-link-target"><span>Slovenščina</span></a></li><li class="interlanguage-link interwiki-sr mw-list-item"><a href="https://sr.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанска кора — српски" lang="sr" hreflang="sr" data-title="Океанска кора" data-language-autonym="Српски / srpski" data-language-local-name="српски" class="interlanguage-link-target"><span>Српски / srpski</span></a></li><li class="interlanguage-link interwiki-sh mw-list-item"><a href="https://sh.wikipedia.org/wiki/Okeanska_kora" title="Okeanska kora — српскохрватски" lang="sh" hreflang="sh" data-title="Okeanska kora" data-language-autonym="Srpskohrvatski / српскохрватски" data-language-local-name="српскохрватски" class="interlanguage-link-target"><span>Srpskohrvatski / српскохрватски</span></a></li><li class="interlanguage-link interwiki-th mw-list-item"><a href="https://th.wikipedia.org/wiki/%E0%B9%80%E0%B8%9B%E0%B8%A5%E0%B8%B7%E0%B8%AD%E0%B8%81%E0%B9%82%E0%B8%A5%E0%B8%81%E0%B8%A0%E0%B8%B2%E0%B8%84%E0%B8%9E%E0%B8%B7%E0%B9%89%E0%B8%99%E0%B8%AA%E0%B8%A1%E0%B8%B8%E0%B8%97%E0%B8%A3" title="เปลือกโลกภาคพื้นสมุทร — тајландски" lang="th" hreflang="th" data-title="เปลือกโลกภาคพื้นสมุทร" data-language-autonym="ไทย" data-language-local-name="тајландски" class="interlanguage-link-target"><span>ไทย</span></a></li><li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://tr.wikipedia.org/wiki/Okyanusal_kabuk" title="Okyanusal kabuk — турски" lang="tr" hreflang="tr" data-title="Okyanusal kabuk" data-language-autonym="Türkçe" data-language-local-name="турски" class="interlanguage-link-target"><span>Türkçe</span></a></li><li class="interlanguage-link interwiki-uk mw-list-item"><a href="https://uk.wikipedia.org/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%96%D1%87%D0%BD%D0%B0_%D0%B7%D0%B5%D0%BC%D0%BD%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Океанічна земна кора — украински" lang="uk" hreflang="uk" data-title="Океанічна земна кора" data-language-autonym="Українська" data-language-local-name="украински" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-vec mw-list-item"><a href="https://vec.wikipedia.org/wiki/Crosta_ose%C3%A0nega" title="Crosta oseànega — венетски" lang="vec" hreflang="vec" data-title="Crosta oseànega" data-language-autonym="Vèneto" data-language-local-name="венетски" class="interlanguage-link-target"><span>Vèneto</span></a></li><li class="interlanguage-link interwiki-vi mw-list-item"><a href="https://vi.wikipedia.org/wiki/V%E1%BB%8F_%C4%91%E1%BA%A1i_d%C6%B0%C6%A1ng" title="Vỏ đại dương — виетнамски" lang="vi" hreflang="vi" data-title="Vỏ đại dương" data-language-autonym="Tiếng Việt" data-language-local-name="виетнамски" class="interlanguage-link-target"><span>Tiếng Việt</span></a></li><li class="interlanguage-link interwiki-zh mw-list-item"><a href="https://zh.wikipedia.org/wiki/%E6%B5%B7%E6%B4%8B%E5%9C%B0%E6%AE%BC" title="海洋地殼 — кинески" lang="zh" hreflang="zh" data-title="海洋地殼" data-language-autonym="中文" data-language-local-name="кинески" class="interlanguage-link-target"><span>中文</span></a></li><li class="interlanguage-link interwiki-kge mw-list-item"><a href="https://kge.wikipedia.org/wiki/Korak_Samudra" title="Korak Samudra — Komering" lang="kge" hreflang="kge" data-title="Korak Samudra" data-language-autonym="Kumoring" data-language-local-name="Komering" class="interlanguage-link-target"><span>Kumoring</span></a></li> </ul> <div class="after-portlet after-portlet-lang"><span class="wb-langlinks-edit wb-langlinks-link"><a href="https://www.wikidata.org/wiki/Special:EntityPage/Q238851#sitelinks-wikipedia" title="Уредување на меѓујазични врски" class="wbc-editpage">Уреди врски</a></span></div> </div> </div> </div> </header> <div class="vector-page-toolbar"> <div class="vector-page-toolbar-container"> <div id="left-navigation"> <nav aria-label="Именски простори"> <div id="p-associated-pages" class="vector-menu vector-menu-tabs mw-portlet mw-portlet-associated-pages" > <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li id="ca-nstab-main" class="selected vector-tab-noicon mw-list-item"><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Преглед на содржинската страница [c]" accesskey="c"><span>Страница</span></a></li><li id="ca-talk" class="vector-tab-noicon mw-list-item"><a href="/wiki/%D0%A0%D0%B0%D0%B7%D0%B3%D0%BE%D0%B2%D0%BE%D1%80:%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" rel="discussion" title="Разговор за содржинската страница [t]" accesskey="t"><span>Разговор</span></a></li> </ul> </div> </div> <div id="vector-variants-dropdown" class="vector-dropdown emptyPortlet" > <input type="checkbox" id="vector-variants-dropdown-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-variants-dropdown" class="vector-dropdown-checkbox " aria-label="Менување на јазичната варијанта" > <label id="vector-variants-dropdown-label" for="vector-variants-dropdown-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet" aria-hidden="true" ><span class="vector-dropdown-label-text">македонски</span> </label> <div class="vector-dropdown-content"> <div id="p-variants" class="vector-menu mw-portlet mw-portlet-variants emptyPortlet" > <div class="vector-menu-content"> <ul class="vector-menu-content-list"> </ul> </div> </div> </div> </div> </nav> </div> <div id="right-navigation" class="vector-collapsible"> <nav aria-label="Посети"> <div id="p-views" class="vector-menu vector-menu-tabs mw-portlet mw-portlet-views" > <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li id="ca-view" class="selected vector-tab-noicon mw-list-item"><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0"><span>Читај</span></a></li><li id="ca-ve-edit" class="vector-tab-noicon mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit" title="Уредете ја страницава [v]" accesskey="v"><span>Уреди</span></a></li><li id="ca-edit" class="collapsible vector-tab-noicon mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit" title="Уредување на изворниот код на страницава [e]" accesskey="e"><span>Уреди извор</span></a></li><li id="ca-history" class="vector-tab-noicon mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=history" title="Претходни верзии на оваа страница. [h]" accesskey="h"><span>Историја</span></a></li> </ul> </div> </div> </nav> <nav class="vector-page-tools-landmark" aria-label="Алатки за страници"> <div id="vector-page-tools-dropdown" class="vector-dropdown vector-page-tools-dropdown" > <input type="checkbox" id="vector-page-tools-dropdown-checkbox" role="button" aria-haspopup="true" data-event-name="ui.dropdown-vector-page-tools-dropdown" class="vector-dropdown-checkbox " aria-label="алатник" > <label id="vector-page-tools-dropdown-label" for="vector-page-tools-dropdown-checkbox" class="vector-dropdown-label cdx-button cdx-button--fake-button cdx-button--fake-button--enabled cdx-button--weight-quiet" aria-hidden="true" ><span class="vector-dropdown-label-text">алатник</span> </label> <div class="vector-dropdown-content"> <div id="vector-page-tools-unpinned-container" class="vector-unpinned-container"> <div id="vector-page-tools" class="vector-page-tools vector-pinnable-element"> <div class="vector-pinnable-header vector-page-tools-pinnable-header vector-pinnable-header-unpinned" data-feature-name="page-tools-pinned" data-pinnable-element-id="vector-page-tools" data-pinned-container-id="vector-page-tools-pinned-container" data-unpinned-container-id="vector-page-tools-unpinned-container" > <div class="vector-pinnable-header-label">Алатки</div> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-pin-button" data-event-name="pinnable-header.vector-page-tools.pin">премести во страничникот</button> <button class="vector-pinnable-header-toggle-button vector-pinnable-header-unpin-button" data-event-name="pinnable-header.vector-page-tools.unpin">скриј</button> </div> <div id="p-cactions" class="vector-menu mw-portlet mw-portlet-cactions emptyPortlet vector-has-collapsible-items" title="Повеќе можности" > <div class="vector-menu-heading"> Дејства </div> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li id="ca-more-view" class="selected vector-more-collapsible-item mw-list-item"><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0"><span>Читај</span></a></li><li id="ca-more-ve-edit" class="vector-more-collapsible-item mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit" title="Уредете ја страницава [v]" accesskey="v"><span>Уреди</span></a></li><li id="ca-more-edit" class="collapsible vector-more-collapsible-item mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit" title="Уредување на изворниот код на страницава [e]" accesskey="e"><span>Уреди извор</span></a></li><li id="ca-more-history" class="vector-more-collapsible-item mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=history"><span>Историја</span></a></li> </ul> </div> </div> <div id="p-tb" class="vector-menu mw-portlet mw-portlet-tb" > <div class="vector-menu-heading"> Општо </div> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li id="t-whatlinkshere" class="mw-list-item"><a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%A8%D1%82%D0%BE%D0%92%D0%BE%D0%B4%D0%B8%D0%9E%D0%B2%D0%B4%D0%B5/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Список на сите викистраници што водат овде [j]" accesskey="j"><span>Што води овде</span></a></li><li id="t-recentchangeslinked" class="mw-list-item"><a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%BE%D0%B2%D1%80%D0%B7%D0%B0%D0%BD%D0%B8%D0%9F%D1%80%D0%BE%D0%BC%D0%B5%D0%BD%D0%B8/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" rel="nofollow" title="Скорешни промени на страници со врски на оваа страница [k]" accesskey="k"><span>Поврзани промени</span></a></li><li id="t-specialpages" class="mw-list-item"><a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%A1%D0%BB%D1%83%D0%B6%D0%B1%D0%B5%D0%BD%D0%B8%D0%A1%D1%82%D1%80%D0%B0%D0%BD%D0%B8%D1%86%D0%B8" title="Список на сите службени страници [q]" accesskey="q"><span>Службени страници</span></a></li><li id="t-permalink" class="mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&oldid=5251830" title="Постојана врска до оваа преработка на страницата"><span>Постојана врска</span></a></li><li id="t-info" class="mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=info" title="Повеќе информации за страницата"><span>Информации за страницата</span></a></li><li id="t-cite" class="mw-list-item"><a href="/w/index.php?title=%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9D%D0%B0%D0%B2%D0%BE%D0%B4&page=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&id=5251830&wpFormIdentifier=titleform" title="Информации како да ја наведете оваа страница"><span>Наведи ја страницава</span></a></li><li id="t-urlshortener" class="mw-list-item"><a href="/w/index.php?title=%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%A1%D0%BA%D1%80%D0%B0%D1%82%D1%83%D0%B2%D0%B0%D1%87%D0%9D%D0%B0URL&url=https%3A%2F%2Fmk.wikipedia.org%2Fwiki%2F%25D0%259E%25D0%25BA%25D0%25B5%25D0%25B0%25D0%25BD%25D1%2581%25D0%25BA%25D0%25B0_%25D0%25BA%25D0%25BE%25D1%2580%25D0%25B0"><span>Дај скратена URL</span></a></li><li id="t-urlshortener-qrcode" class="mw-list-item"><a href="/w/index.php?title=%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:QrCode&url=https%3A%2F%2Fmk.wikipedia.org%2Fwiki%2F%25D0%259E%25D0%25BA%25D0%25B5%25D0%25B0%25D0%25BD%25D1%2581%25D0%25BA%25D0%25B0_%25D0%25BA%25D0%25BE%25D1%2580%25D0%25B0"><span>Преземи QR-код</span></a></li> </ul> </div> </div> <div id="p-coll-print_export" class="vector-menu mw-portlet mw-portlet-coll-print_export" > <div class="vector-menu-heading"> Печати/извези </div> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li id="coll-create_a_book" class="mw-list-item"><a href="/w/index.php?title=%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9A%D0%BD%D0%B8%D0%B3%D0%B0&bookcmd=book_creator&referer=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0"><span>Создај книга</span></a></li><li id="coll-download-as-rl" class="mw-list-item"><a href="/w/index.php?title=%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:DownloadAsPdf&page=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=show-download-screen"><span>Преземи како PDF</span></a></li><li id="t-print" class="mw-list-item"><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&printable=yes" title="Верзија за печатење на оваа страница [p]" accesskey="p"><span>Верзија за печатење</span></a></li> </ul> </div> </div> <div id="p-wikibase-otherprojects" class="vector-menu mw-portlet mw-portlet-wikibase-otherprojects" > <div class="vector-menu-heading"> На други проекти </div> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="wb-otherproject-link wb-otherproject-commons mw-list-item"><a href="https://commons.wikimedia.org/wiki/Category:Plate_tectonics" hreflang="en"><span>Ризница</span></a></li><li id="t-wikibase" class="wb-otherproject-link 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dir="ltr"><figure typeof="mw:File/Thumb"><a href="/wiki/%D0%9F%D0%BE%D0%B4%D0%B0%D1%82%D0%BE%D1%82%D0%B5%D0%BA%D0%B0:2008_age_of_oceans_plates.jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/2008_age_of_oceans_plates.jpg/300px-2008_age_of_oceans_plates.jpg" decoding="async" width="300" height="180" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/2008_age_of_oceans_plates.jpg/450px-2008_age_of_oceans_plates.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/e/e7/2008_age_of_oceans_plates.jpg/600px-2008_age_of_oceans_plates.jpg 2x" data-file-width="2560" data-file-height="1539" /></a><figcaption>Боите ја означуваат возраста на океанската кора, каде што поцрвеното означува помлада возраст, а посиното означува постара возраст. Линиите ги претставуваат границите на тектонските плочи.</figcaption></figure> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/%D0%9F%D0%BE%D0%B4%D0%B0%D1%82%D0%BE%D1%82%D0%B5%D0%BA%D0%B0:Continental_and_oceanic_crust_mk.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/d/da/Continental_and_oceanic_crust_mk.png/220px-Continental_and_oceanic_crust_mk.png" decoding="async" width="220" height="133" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/da/Continental_and_oceanic_crust_mk.png/330px-Continental_and_oceanic_crust_mk.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/da/Continental_and_oceanic_crust_mk.png/440px-Continental_and_oceanic_crust_mk.png 2x" data-file-width="2887" data-file-height="1750" /></a><figcaption>Континентална и океанска кора на горната обвивка на Земјата</figcaption></figure> <p><b>Океанската кора</b> — најгорниот слој на океанскиот дел од <a href="/wiki/%D0%A2%D0%B5%D0%BA%D1%82%D0%BE%D0%BD%D0%B8%D0%BA%D0%B0_%D0%BD%D0%B0_%D0%BF%D0%BB%D0%BE%D1%87%D0%B8%D1%82%D0%B5" title="Тектоника на плочите">тектонските плочи</a>. Таа е составена од горната океанска кора, со <a href="/wiki/%D0%9F%D0%B5%D1%80%D0%BD%D0%B8%D1%87%D0%B5%D1%81%D1%82%D0%B0_%D0%BB%D0%B0%D0%B2%D0%B0" title="Перничеста лава">перничеста лава</a> и комплекс на насипи, и долната океанска кора, составена од <a href="/w/index.php?title=%D0%A2%D1%80%D0%BE%D0%BA%D1%82%D0%BE%D0%BB%D0%B8%D1%82&action=edit&redlink=1" class="new" title="Троктолит (страницата не постои)">троктолит</a>, <a href="/wiki/%D0%93%D0%B0%D0%B1%D1%80%D0%BE" title="Габро">габро</a> и <a href="/w/index.php?title=%D0%A3%D0%BB%D1%82%D1%80%D0%B0%D0%BC%D0%B0%D1%84%D0%B8%D1%87%D0%BD%D0%B0_%D0%BA%D0%B0%D1%80%D0%BF%D0%B0&action=edit&redlink=1" class="new" title="Ултрамафична карпа (страницата не постои)">ултрамафични карпи</a>.<sup id="cite_ref-Gillis_2014_1-0" class="reference"><a href="#cite_note-Gillis_2014-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-Pirajno_2013_2-0" class="reference"><a href="#cite_note-Pirajno_2013-2"><span class="cite-bracket">[</span>2<span class="cite-bracket">]</span></a></sup> Кората се покрива над зацврстениот и најгорниот слој на <a href="/wiki/%D0%9F%D0%BB%D0%B0%D1%88%D1%82_(%D0%B3%D0%B5%D0%BE%D0%BB%D0%BE%D0%B3%D0%B8%D1%98%D0%B0)" title="Плашт (геологија)">плаштот</a>. Кората и цврстиот слој на обвивката заедно ја сочинуваат океанската <a href="/wiki/%D0%9B%D0%B8%D1%82%D0%BE%D1%81%D1%84%D0%B5%D1%80%D0%B0" title="Литосфера">литосфера</a>. </p><p>Океанската кора е првенствено составена од <a href="/w/index.php?title=%D0%9C%D0%B0%D1%84%D0%B8%D1%87%D0%BD%D0%BE%D1%81%D1%82&action=edit&redlink=1" class="new" title="Мафичност (страницата не постои)">мафични карпи</a>, или <a href="/w/index.php?title=%D0%A1%D0%B8%D0%BC%D0%B0_(%D0%B3%D0%B5%D0%BE%D0%BB%D0%BE%D0%B3%D0%B8%D1%98%D0%B0)&action=edit&redlink=1" class="new" title="Сима (геологија) (страницата не постои)">сима</a>, која е богата со <a href="/wiki/%D0%96%D0%B5%D0%BB%D0%B5%D0%B7%D0%BE" title="Железо">железо</a> и <a href="/wiki/%D0%9C%D0%B0%D0%B3%D0%BD%D0%B5%D0%B7%D0%B8%D1%83%D0%BC" title="Магнезиум">магнезиум</a>. Таа е потенка од <a href="/wiki/%D0%9A%D0%BE%D0%BD%D1%82%D0%B8%D0%BD%D0%B5%D0%BD%D1%82%D0%B0%D0%BB%D0%BD%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Континентална кора">континенталната кора</a>, генерално дебела помала од 10 километри; сепак, таа е погуста, имајќи средна густина од околу 3,0 <a href="/wiki/%D0%93%D1%80%D0%B0%D0%BC" title="Грам">грама</a> на кубен сантиметар за разлика од континенталната кора која има густина од околу 2,7 грама на кубен сантиметар.<sup id="cite_ref-Cogley-1984_3-0" class="reference"><a href="#cite_note-Cogley-1984-3"><span class="cite-bracket">[</span>3<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-Rogers_4-0" class="reference"><a href="#cite_note-Rogers-4"><span class="cite-bracket">[</span>4<span class="cite-bracket">]</span></a></sup> </p><p>Најгорната кора е резултат на ладењето на магмата добиена од материјалот на плаштот под плочата. Магмата се вбризгува во центарот за ширење, кој главно се состои од делумно зацврстена <a href="/w/index.php?title=%D0%9A%D1%80%D0%B8%D1%81%D1%82%D0%B0%D0%BB%D0%BD%D0%B0_%D0%BA%D0%B0%D1%88%D0%B0&action=edit&redlink=1" class="new" title="Кристална каша (страницата не постои)">кристална каша</a>, формирајќи леќи од магма кои се извор на <a href="/w/index.php?title=%D0%9A%D0%BE%D0%BC%D0%BF%D0%BB%D0%B5%D0%BA%D1%81_%D1%81%D0%BE_%D1%87%D0%B0%D1%80%D1%88%D0%B0%D1%84%D0%B8&action=edit&redlink=1" class="new" title="Комплекс со чаршафи (страницата не постои)">обложените насипи</a> кои ги хранат лавата на прекриените перници.<sup id="cite_ref-Sinton_&_Detrick_5-0" class="reference"><a href="#cite_note-Sinton_&_Detrick-5"><span class="cite-bracket">[</span>5<span class="cite-bracket">]</span></a></sup> Како што лавата се лади, тие, во повеќето случаи, се хемиски модифицирани со морска вода.<sup id="cite_ref-6" class="reference"><a href="#cite_note-6"><span class="cite-bracket">[</span>6<span class="cite-bracket">]</span></a></sup> Овие ерупции се случуваат најмногу на сртовите на средината на океанот, но исто така и на расфрлани жаришта, а исто така и во ретки, но моќни појави познати како ерупции на поплавен балзат. Но, повеќето <a href="/wiki/%D0%9C%D0%B0%D0%B3%D0%BC%D0%B0" title="Магма">магми</a> се <a href="/w/index.php?title=%D0%9A%D1%80%D0%B8%D1%81%D1%82%D0%B0%D0%BB%D0%B8%D0%B7%D0%B0%D1%86%D0%B8%D1%98%D0%B0&action=edit&redlink=1" class="new" title="Кристализација (страницата не постои)">кристализираат</a> на длабочина, во <a href="/w/index.php?title=%D0%94%D0%BE%D0%BB%D0%BD%D0%B0_%D0%BE%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&redlink=1" class="new" title="Долна океанска кора (страницата не постои)">долната океанска кора</a>. Таму, новонападната магма може да се меша и да реагира со претходно постоечка кристална каша и карпи.<sup id="cite_ref-7" class="reference"><a href="#cite_note-7"><span class="cite-bracket">[</span>7<span class="cite-bracket">]</span></a></sup> </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Состав"><span id=".D0.A1.D0.BE.D1.81.D1.82.D0.B0.D0.B2"></span>Состав</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit&section=1" title="Уреди го одделот „Состав“" class="mw-editsection-visualeditor"><span>уреди</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&section=1" title="Уреди изворен код на одделот: Состав"><span>уреди извор</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Иако целосен дел од океанската кора сè уште не е пробиен, геолозите имаат неколку докази кои им помагаат да го разберат океанското дно. Проценките на составот се засноваат на анализи на <a href="/w/index.php?title=%D0%9E%D1%84%D0%B8%D0%BE%D0%BB%D0%B8%D1%82&action=edit&redlink=1" class="new" title="Офиолит (страницата не постои)">офиолит</a> (делови од океанската кора што се зачувани на континентите), споредби на <a href="/wiki/%D0%A1%D0%B5%D0%B8%D0%B7%D0%BC%D0%BE%D0%BB%D0%BE%D0%B3%D0%B8%D1%98%D0%B0" title="Сеизмологија">сеизмичката структура</a> на океанската кора со лабораториски определби на сеизмичките брзини кај познати типови карпи и примероци добиени од океанското дно.<sup id="cite_ref-8" class="reference"><a href="#cite_note-8"><span class="cite-bracket">[</span>8<span class="cite-bracket">]</span></a></sup> Океанската кора е значително поедноставна од континенталната кора и генерално може да се подели на три слоја.<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">[</span>9<span class="cite-bracket">]</span></a></sup> Според експериментите со <a href="/w/index.php?title=%D0%9C%D0%B8%D0%BD%D0%B5%D1%80%D0%B0%D0%BB%D0%BD%D0%B0_%D1%84%D0%B8%D0%B7%D0%B8%D0%BA%D0%B0&action=edit&redlink=1" class="new" title="Минерална физика (страницата не постои)">минерална физика</a>, при пониски притисоци на обвивката, океанската кора станува погуста од околната обвивка.<sup id="cite_ref-10" class="reference"><a href="#cite_note-10"><span class="cite-bracket">[</span>10<span class="cite-bracket">]</span></a></sup> </p> <ul><li><b>Слој 1</b> е во просек 0,4 км дебелина. Се состои од неконсолидирани или полуконсолидирани седименти, обично тенки или дури не присутни во близина на средноокеанските гребени, но се згуснуваат подалеку од гребенот.<sup id="cite_ref-11" class="reference"><a href="#cite_note-11"><span class="cite-bracket">[</span>11<span class="cite-bracket">]</span></a></sup> Во близина на континенталните рабови седиментот е териген, што значи дека потекнува од копно, за разлика од длабокоморските седименти кои се направени од ситни <a href="/wiki/%D0%95%D0%B3%D0%B7%D0%BE%D1%81%D0%BA%D0%B5%D0%BB%D0%B5%D1%82" title="Егзоскелет">лушпи</a> од морски организми, обично варовнички и силикозни, или може да бидат направени од <a href="/wiki/%D0%92%D1%83%D0%BB%D0%BA%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BF%D0%B5%D0%BF%D0%B5%D0%BB" class="mw-redirect" title="Вулканска пепел">вулканска пепел</a> и теригени седименти транспортирани со заматени струји.<sup id="cite_ref-12" class="reference"><a href="#cite_note-12"><span class="cite-bracket">[</span>12<span class="cite-bracket">]</span></a></sup></li> <li><b>Слој 2</b> може да се подели на два дела: слој 2А – 0,5 км дебел најгорниот вулкански слој од стаклен до ситно кристален <a href="/wiki/%D0%91%D0%B0%D0%B7%D0%B0%D0%BB%D1%82" title="Базалт">базалт</a> обично во форма на <a href="/wiki/%D0%9F%D0%B5%D1%80%D0%BD%D0%B8%D1%87%D0%B5%D1%81%D1%82%D0%B0_%D0%BB%D0%B0%D0%B2%D0%B0" title="Перничеста лава">перничеста лава</a> и слој 2B – 1,5 km дебел слој составен од <a href="/wiki/%D0%94%D0%B8%D1%98%D0%B0%D0%B1%D0%B0%D0%B7" title="Дијабаз">дијабазни</a> насипи.<sup id="cite_ref-13" class="reference"><a href="#cite_note-13"><span class="cite-bracket">[</span>13<span class="cite-bracket">]</span></a></sup></li> <li><b>Слој 3</b> се формира со бавно ладење на <a href="/wiki/%D0%9C%D0%B0%D0%B3%D0%BC%D0%B0" title="Магма">магмата</a> под површината и се состои од крупно зрнести <a href="/wiki/%D0%93%D0%B0%D0%B1%D1%80%D0%BE" title="Габро">габроси</a> и кумулирани ултрамафни карпи.<sup id="cite_ref-Gillis_2014_1-1" class="reference"><a href="#cite_note-Gillis_2014-1"><span class="cite-bracket">[</span>1<span class="cite-bracket">]</span></a></sup> Сочинува над две третини од волуменот на океанската кора со речиси 5 км дебелина.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">[</span>14<span class="cite-bracket">]</span></a></sup></li></ul> <div class="mw-heading mw-heading3"><h3 id="Геохемија"><span id=".D0.93.D0.B5.D0.BE.D1.85.D0.B5.D0.BC.D0.B8.D1.98.D0.B0"></span>Геохемија</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit&section=2" title="Уреди го одделот „Геохемија“" class="mw-editsection-visualeditor"><span>уреди</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&section=2" title="Уреди изворен код на одделот: Геохемија"><span>уреди извор</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Најобемните <a href="/w/index.php?title=%D0%92%D1%83%D0%BB%D0%BA%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%B0%D1%80%D0%BF%D0%B0&action=edit&redlink=1" class="new" title="Вулканска карпа (страницата не постои)">вулкански карпи</a> на океанското дно се базалтите од средноокеански гребени, кои потекнуваат од <a href="/w/index.php?title=%D0%A2%D0%BE%D0%BB%D0%B5%D0%B8%D1%82%D0%B8%D0%BD%D1%81%D0%BA%D0%B0_%D0%BC%D0%B0%D0%B3%D0%BC%D0%B0_%D1%81%D0%B5%D1%80%D0%B8%D1%98%D0%B0&action=edit&redlink=1" class="new" title="Толеитинска магма серија (страницата не постои)">толеитски магми</a> со ниска содржина на <a href="/wiki/%D0%9A%D0%B0%D0%BB%D0%B8%D1%83%D0%BC" title="Калиум">калиум</a>. Овие карпи имаат ниски концентрации на големи јонски литофилни елементи, лесни ретки земјени елементи, испарливи елементи и други многу некомпатибилни елементи. Може да се најдат базалти збогатени со некомпатибилни елементи, но тие се ретки и се поврзани со <a href="/wiki/%D0%92%D1%80%D0%B5%D0%BB%D0%B0_%D1%82%D0%BE%D1%87%D0%BA%D0%B0" title="Врела точка">жариштата</a> на средишниот океански гребен, како што се околината на <a href="/wiki/%D0%93%D0%B0%D0%BB%D0%B0%D0%BF%D0%B0%D0%B3%D0%BE%D1%81" title="Галапагос">островите Галапагос</a>, <a href="/wiki/%D0%90%D0%B7%D0%BE%D1%80%D0%B8" title="Азори">Азорите</a> и <a href="/wiki/%D0%98%D1%81%D0%BB%D0%B0%D0%BD%D0%B4" title="Исланд">Исланд</a>.<sup id="cite_ref-15" class="reference"><a href="#cite_note-15"><span class="cite-bracket">[</span>15<span class="cite-bracket">]</span></a></sup> </p><p>Пред ерата на неопротерозоикот, пред 1000 Ма, светската океанска кора била <a href="/wiki/%D0%9C%D0%B5%D0%B3%D0%B0%D0%B3%D0%BE%D0%B4%D0%B8%D0%BD%D0%B0" title="Мегагодина">помафична</a> отколку денешнава. Помафичната природа на кората значело дека поголеми количини на молекули на вода (<a href="/wiki/%D0%A5%D0%B8%D0%B4%D1%80%D0%BE%D0%BA%D1%81%D0%B8%D0%BB%D0%BD%D0%B0_%D0%B3%D1%80%D1%83%D0%BF%D0%B0" class="mw-redirect" title="Хидроксилна група">OH</a>) може да се складираат во изменетите делови од кората. Во зоните на подвлекување, оваа мафична кора била склона да се метаморфозира во зелени шкрилци.<sup id="cite_ref-PaWh2016_16-0" class="reference"><a href="#cite_note-PaWh2016-16"><span class="cite-bracket">[</span>16<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Животен_циклус"><span id=".D0.96.D0.B8.D0.B2.D0.BE.D1.82.D0.B5.D0.BD_.D1.86.D0.B8.D0.BA.D0.BB.D1.83.D1.81"></span>Животен циклус</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit&section=3" title="Уреди го одделот „Животен циклус“" class="mw-editsection-visualeditor"><span>уреди</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&section=3" title="Уреди изворен код на одделот: Животен циклус"><span>уреди извор</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Океанската кора континуирано се создава на средноокеанските сртови. Како што <a href="/wiki/%D0%A2%D0%B5%D0%BA%D1%82%D0%BE%D0%BD%D0%B8%D0%BA%D0%B0_%D0%BD%D0%B0_%D0%BF%D0%BB%D0%BE%D1%87%D0%B8%D1%82%D0%B5" title="Тектоника на плочите">континенталните плочи</a> се разминуваат на овие гребени, магмата се издигнува во горната обвивка и кората. Како што континенталните плочи се оддалечуваат од гребенот, новосоздадените карпи се ладат и почнуваат да еродираат со седимент кој постепено се собира врз нив. Најмладите океански карпи се наоѓаат во океанските гребени и тие постепено стареат далеку од гребените.<sup id="cite_ref-17" class="reference"><a href="#cite_note-17"><span class="cite-bracket">[</span>17<span class="cite-bracket">]</span></a></sup> </p><p>Како што наметката се крева, таа се лади и се топи, додека притисокот се намалува и го преминува солидусот. Количината на произведеното топење зависи само од температурата на обвивката додека се зголемува. Оттука, поголемиот дел од океанската кора е со иста дебелина (7±1 км). Сртови со многу бавно ширење (<1 см·год. <sup>−1</sup> полустапка) произведуваат потенка кора (4–5 км дебелина) бидејќи обвивката има можност да се олади при издигнување и така поминува низ цврстината и се топи на помала длабочина, а со тоа создава помалку топење и потенка кора. Пример за ова е гребенот Гакел под <a href="/wiki/%D0%A1%D0%B5%D0%B2%D0%B5%D1%80%D0%BD%D0%BE%D0%BB%D0%B5%D0%B4%D0%B5%D0%BD_%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD" title="Северноледен Океан">Северноледениот Океан</a>. Подебела од просечната кора се наоѓа над облаците бидејќи обвивката е потопла и оттаму ја преминува цврстината и се топи на поголема длабочина, создавајќи повеќе топење и подебела кора. Пример за ова е <a href="/wiki/%D0%98%D1%81%D0%BB%D0%B0%D0%BD%D0%B4" title="Исланд">Исланд</a> кој има кора со дебелина ~20 км. </p><p>Староста на океанската кора може да се користи за да се процени топлинската дебелина на литосферата, каде што младата океанска кора немала доволно време да ја олади плаштот под неа, додека постарата океанска кора има подебела литосфера на плаштот под неа.<sup id="cite_ref-18" class="reference"><a href="#cite_note-18"><span class="cite-bracket">[</span>18<span class="cite-bracket">]</span></a></sup> Океанската литосфера се спушта на она што е познато како конвергентни граници. Овие граници може да постојат помеѓу океанската литосфера на една плоча и океанската литосфера на друга, или помеѓу океанската литосфера на една плоча и континенталната литосфера на друга. Во втората ситуација, океанската литосфера секогаш се спушта бидејќи континенталната литосфера е помалку густа. Процесот на подвлекување троши постара океанска литосфера, така што океанската кора ретко е стара повеќе од 200 милиони години.<sup id="cite_ref-19" class="reference"><a href="#cite_note-19"><span class="cite-bracket">[</span>19<span class="cite-bracket">]</span></a></sup> Процесот на формирање и уништување на супер-континент преку повторени циклуси на создавање и уништување на океанската кора е познат како <a href="/w/index.php?title=%D0%A6%D0%B8%D0%BA%D0%BB%D1%83%D1%81_%D0%92%D0%B8%D0%BB%D1%81%D0%BE%D0%BD&action=edit&redlink=1" class="new" title="Циклус Вилсон (страницата не постои)">Вилсоновиот циклус</a>. </p><p>Најстарата океанска кора од големи размери е во западниот <a href="/wiki/%D0%A2%D0%B8%D1%85%D0%B8_%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD" title="Тихи Океан">Тихи Океан</a> и северозападниот <a href="/wiki/%D0%90%D1%82%D0%BB%D0%B0%D0%BD%D1%82%D1%81%D0%BA%D0%B8_%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD" title="Атлантски Океан">Атлантик</a> - и двете се стари околу 180-200 милиони години. Сепак, делови од источното <a href="/wiki/%D0%A1%D1%80%D0%B5%D0%B4%D0%BE%D0%B7%D0%B5%D0%BC%D0%BD%D0%BE_%D0%9C%D0%BE%D1%80%D0%B5" title="Средоземно Море">Средоземно Море</a> би можеле да бидат остатоци од многу постариот океан Тетис, стар околу 270 и до 340 милиони години.<sup id="cite_ref-20" class="reference"><a href="#cite_note-20"><span class="cite-bracket">[</span>20<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-21" class="reference"><a href="#cite_note-21"><span class="cite-bracket">[</span>21<span class="cite-bracket">]</span></a></sup><sup id="cite_ref-22" class="reference"><a href="#cite_note-22"><span class="cite-bracket">[</span>22<span class="cite-bracket">]</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Магнетни_аномалии"><span id=".D0.9C.D0.B0.D0.B3.D0.BD.D0.B5.D1.82.D0.BD.D0.B8_.D0.B0.D0.BD.D0.BE.D0.BC.D0.B0.D0.BB.D0.B8.D0.B8"></span>Магнетни аномалии</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit&section=4" title="Уреди го одделот „Магнетни аномалии“" class="mw-editsection-visualeditor"><span>уреди</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&section=4" title="Уреди изворен код на одделот: Магнетни аномалии"><span>уреди извор</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Океанската кора прикажува шема на магнетни линии, паралелни со океанските гребени, замрзнати во <a href="/wiki/%D0%91%D0%B0%D0%B7%D0%B0%D0%BB%D1%82" title="Базалт">базалтот</a>. Симетрична шема на позитивни и негативни магнетни линии произлегува од средноокеанскиот гребен.<sup id="cite_ref-23" class="reference"><a href="#cite_note-23"><span class="cite-bracket">[</span>23<span class="cite-bracket">]</span></a></sup> Новата карпа е формирана од магмата на сртовите на средината на океанот, а океанското дно се шири од оваа точка. Кога магмата се лади за да формира карпа, нејзиниот магнетен поларитет е усогласен со тогашните сегашни позиции на магнетните полови на Земјата. Новата магма потоа ја принудува постарата оладена магма да се оддалечи од гребенот. Овој процес резултира со паралелни делови од океанската кора со наизменичен магнетен поларитет. </p> <div class="mw-heading mw-heading2"><h2 id="Наводи"><span id=".D0.9D.D0.B0.D0.B2.D0.BE.D0.B4.D0.B8"></span>Наводи</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit&section=5" title="Уреди го одделот „Наводи“" class="mw-editsection-visualeditor"><span>уреди</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&section=5" title="Уреди изворен код на одделот: Наводи"><span>уреди извор</span></a><span class="mw-editsection-bracket">]</span></span></div> <div class="reflist" style="list-style-type: decimal;"> <div class="mw-references-wrap mw-references-columns"><ol class="references"> <li id="cite_note-Gillis_2014-1"><span class="mw-cite-backlink">↑ <sup><a href="#cite_ref-Gillis_2014_1-0">1,0</a></sup> <sup><a href="#cite_ref-Gillis_2014_1-1">1,1</a></sup></span> <span class="reference-text">Gillis et al (2014). Primitive layered gabbros from fast-spreading lower oceanic crust. Nature 505, 204-208</span> </li> <li id="cite_note-Pirajno_2013-2"><span class="mw-cite-backlink"><a href="#cite_ref-Pirajno_2013_2-0">↑</a></span> <span class="reference-text"><cite id="CITEREFPirajno_F.2013" class="citation book">Pirajno F. (2013). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=PrXyCAAAQBAJ&q=ultramafic+cumulates+layer+3&pg=PA11"><i>Ore Deposits and Mantle Plumes</i></a>. Springer. стр. 11. <a href="/wiki/ISBN" title="ISBN">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/9789401725026" title="Специјална:ПечатенИзвор/9789401725026"><bdi>9789401725026</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=Ore+Deposits+and+Mantle+Plumes&rft.pages=11&rft.pub=Springer&rft.date=2013&rft.isbn=9789401725026&rft.au=Pirajno+F.&rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3DPrXyCAAAQBAJ%26q%3Dultramafic%2Bcumulates%2Blayer%2B3%26pg%3DPA11&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><style data-mw-deduplicate="TemplateStyles:r5289462">.mw-parser-output cite.citation{font-style:inherit}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .id-lock-free a,.mw-parser-output .citation .cs1-lock-free a{background-image:url("//upload.wikimedia.org/wikipedia/commons/thumb/6/65/Lock-green.svg/9px-Lock-green.svg.png");background-image:linear-gradient(transparent,transparent),url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg");background-repeat:no-repeat;background-size:9px;background-position:right .1em center}.mw-parser-output .id-lock-limited a,.mw-parser-output .id-lock-registration a,.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration a{background-image:url("//upload.wikimedia.org/wikipedia/commons/thumb/d/d6/Lock-gray-alt-2.svg/9px-Lock-gray-alt-2.svg.png");background-image:linear-gradient(transparent,transparent),url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg");background-repeat:no-repeat;background-size:9px;background-position:right .1em center}.mw-parser-output .id-lock-subscription a,.mw-parser-output .citation .cs1-lock-subscription a{background-image:url("//upload.wikimedia.org/wikipedia/commons/thumb/a/aa/Lock-red-alt-2.svg/9px-Lock-red-alt-2.svg.png");background-image:linear-gradient(transparent,transparent),url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg");background-repeat:no-repeat;background-size:9px;background-position:right .1em center}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration{color:var(--color-subtle,#54595d)}.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span{border-bottom:1px dotted;cursor:help}.mw-parser-output .cs1-ws-icon a{background-image:url("//upload.wikimedia.org/wikipedia/commons/thumb/4/4c/Wikisource-logo.svg/12px-Wikisource-logo.svg.png");background-image:linear-gradient(transparent,transparent),url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg");background-repeat:no-repeat;background-size:12px;background-position:right .1em center}.mw-parser-output code.cs1-code{color:inherit;background:inherit;border:inherit;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;font-size:100%}.mw-parser-output .cs1-visible-error{font-size:100%}.mw-parser-output .cs1-maint{display:none;color:#33aa33;margin-left:0.3em}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}</style></span> </li> <li id="cite_note-Cogley-1984-3"><span class="mw-cite-backlink"><a href="#cite_ref-Cogley-1984_3-0">↑</a></span> <span class="reference-text"><a href="#CITEREFCogley1984">Cogley 1984</a><span class="error harv-error" style="display: none; font-size:100%"> harvnb error: no target: CITEREFCogley1984 (<a href="/wiki/%D0%9A%D0%B0%D1%82%D0%B5%D0%B3%D0%BE%D1%80%D0%B8%D1%98%D0%B0:Harv_and_Sfn_template_errors" title="Категорија:Harv and Sfn template errors">help</a>)</span></span> </li> <li id="cite_note-Rogers-4"><span class="mw-cite-backlink"><a href="#cite_ref-Rogers_4-0">↑</a></span> <span class="reference-text"><cite id="CITEREFRogers2008" class="citation book">Rogers, N., уред. (2008). <a rel="nofollow" class="external text" href="https://books.google.com/books?id=WA9ST5S_2v0C&pg=PA44"><i>An Introduction to Our Dynamic Planet</i></a>. Cambridge University Press and <a href="/w/index.php?title=The_Open_University&action=edit&redlink=1" class="new" title="The Open University (страницата не постои)">The Open University</a>. стр. 19. <a href="/wiki/ISBN" title="ISBN">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/978-0-521-49424-3" title="Специјална:ПечатенИзвор/978-0-521-49424-3"><bdi>978-0-521-49424-3</bdi></a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=An+Introduction+to+Our+Dynamic+Planet&rft.pages=19&rft.pub=Cambridge+University+Press+and+The+Open+University&rft.date=2008&rft.isbn=978-0-521-49424-3&rft_id=https%3A%2F%2Fbooks.google.com%2Fbooks%3Fid%3DWA9ST5S_2v0C%26pg%3DPA44&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-Sinton_&_Detrick-5"><span class="mw-cite-backlink"><a href="#cite_ref-Sinton_&_Detrick_5-0">↑</a></span> <span class="reference-text"><cite id="CITEREFSinton_J.M.Detrick_R.S.1992" class="citation journal">Sinton J.M.; Detrick R.S. (1992). <a rel="nofollow" class="external text" href="https://www.researchgate.net/publication/248793835">„Mid‐ocean ridge magma chambers“</a>. <i>Journal of Geophysical Research</i>. <b>97</b> (B1): 197–216. <a href="/wiki/Bibcode" title="Bibcode">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1992JGR....97..197S">1992JGR....97..197S</a>. <a href="/wiki/Doi" class="mw-redirect" title="Doi">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1029%2F91JB02508">10.1029/91JB02508</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Journal+of+Geophysical+Research&rft.atitle=Mid%E2%80%90ocean+ridge+magma+chambers&rft.volume=97&rft.issue=B1&rft.pages=197-216&rft.date=1992&rft_id=info%3Adoi%2F10.1029%2F91JB02508&rft_id=info%3Abibcode%2F1992JGR....97..197S&rft.au=Sinton+J.M.&rft.au=Detrick+R.S.&rft_id=https%3A%2F%2Fwww.researchgate.net%2Fpublication%2F248793835&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-6"><span class="mw-cite-backlink"><a href="#cite_ref-6">↑</a></span> <span class="reference-text">H. Elderfield (2006). The Oceans and Marine Geochemistry. Elsevier. pp. 182–. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/978-0-08-045101-5" title="Специјална:ПечатенИзвор/978-0-08-045101-5">978-0-08-045101-5</a>.</span> </li> <li id="cite_note-7"><span class="mw-cite-backlink"><a href="#cite_ref-7">↑</a></span> <span class="reference-text">Lissenberg, C. J., MacLeod, C. J., Horward, K. A., and Godard, M. (2013). Pervasive reactive melt migration through fast-spreading lower oceanic crust (Hess Deep, equatorial Pacific Ocean). Earth Planet. Sci. Lett. 361, 436–447. <a href="/wiki/%D0%9D%D0%B0%D0%B7%D0%BD%D0%B0%D0%BA%D0%B0_%D0%B7%D0%B0_%D0%B4%D0%B8%D0%B3%D0%B8%D1%82%D0%B0%D0%BB%D0%BD%D0%B8_%D0%BE%D0%B1%D1%98%D0%B5%D0%BA%D1%82%D0%B8" title="Назнака за дигитални објекти">doi</a>:<a rel="nofollow" class="external text" href="https://dx.doi.org/10.1016%2Fj.epsl.2012.11.012">10.1016/j.epsl.2012.11.012</a></span> </li> <li id="cite_note-8"><span class="mw-cite-backlink"><a href="#cite_ref-8">↑</a></span> <span class="reference-text">Kodaira, S., Noguchi, N., Takahashi, N., Ishizuka, O., & Kaneda, Y. (2010). Evolution from fore‐arc oceanic crust to island arc crust: A seismic study along the Izu‐Bonin fore arc. <i>Journal of Geophysical Research: Solid Earth,</i> <i>115</i>(B9), N/a.</span> </li> <li id="cite_note-9"><span class="mw-cite-backlink"><a href="#cite_ref-9">↑</a></span> <span class="reference-text"><cite id="CITEREFHansteenTroll2003" class="citation journal">Hansteen, Thor H; Troll, Valentin R (2003-02-14). <a rel="nofollow" class="external text" href="http://www.sciencedirect.com/science/article/pii/S000925410200325X">„Oxygen isotope composition of xenoliths from the oceanic crust and volcanic edifice beneath Gran Canaria (Canary Islands): consequences for crustal contamination of ascending magmas“</a>. <i>Chemical Geology</i> (англиски). <b>193</b> (3): 181–193. <a href="/wiki/Bibcode" title="Bibcode">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2003ChGeo.193..181H">2003ChGeo.193..181H</a>. <a href="/wiki/Doi" class="mw-redirect" title="Doi">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1016%2FS0009-2541%2802%2900325-X">10.1016/S0009-2541(02)00325-X</a>. <a href="/wiki/ISSN" title="ISSN">ISSN</a> <a rel="nofollow" class="external text" href="//www.worldcat.org/issn/0009-2541">0009-2541</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Chemical+Geology&rft.atitle=Oxygen+isotope+composition+of+xenoliths+from+the+oceanic+crust+and+volcanic+edifice+beneath+Gran+Canaria+%28Canary+Islands%29%3A+consequences+for+crustal+contamination+of+ascending+magmas&rft.volume=193&rft.issue=3&rft.pages=181-193&rft.date=2003-02-14&rft.issn=0009-2541&rft_id=info%3Adoi%2F10.1016%2FS0009-2541%2802%2900325-X&rft_id=info%3Abibcode%2F2003ChGeo.193..181H&rft.aulast=Hansteen&rft.aufirst=Thor+H&rft.au=Troll%2C+Valentin+R&rft_id=http%3A%2F%2Fwww.sciencedirect.com%2Fscience%2Farticle%2Fpii%2FS000925410200325X&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-10"><span class="mw-cite-backlink"><a href="#cite_ref-10">↑</a></span> <span class="reference-text">Li, M., & McNamara, A. (2013). The difficulty for subducted oceanic crust to accumulate at the Earth's core‐mantle boundary. <i>Journal of Geophysical Research: Solid Earth,</i> <i>118</i>(4), 1807-1816.</span> </li> <li id="cite_note-11"><span class="mw-cite-backlink"><a href="#cite_ref-11">↑</a></span> <span class="reference-text">Peter Laznicka (2 September 2010). Giant Metallic Deposits: Future Sources of Industrial Metals. Springer Science & Business Media. pp. 82–. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/978-3-642-12405-1" title="Специјална:ПечатенИзвор/978-3-642-12405-1">978-3-642-12405-1</a>.</span> </li> <li id="cite_note-12"><span class="mw-cite-backlink"><a href="#cite_ref-12">↑</a></span> <span class="reference-text">D. R. Bowes (1989) <i>The Encyclopedia of Igneous and Metamorphic Petrology</i>, Van Nostrand Reinhold <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/0-442-20623-2" title="Специјална:ПечатенИзвор/0-442-20623-2">0-442-20623-2</a></span> </li> <li id="cite_note-13"><span class="mw-cite-backlink"><a href="#cite_ref-13">↑</a></span> <span class="reference-text">Yildirim Dilek (1 January 2000). Ophiolites and Oceanic Crust: New Insights from Field Studies and the Ocean Drilling Program. Geological Society of America. pp. 506–. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/978-0-8137-2349-5" title="Специјална:ПечатенИзвор/978-0-8137-2349-5">978-0-8137-2349-5</a>.</span> </li> <li id="cite_note-14"><span class="mw-cite-backlink"><a href="#cite_ref-14">↑</a></span> <span class="reference-text">Jon Erickson (14 May 2014). Plate Tectonics: Unraveling the Mysteries of the Earth. Infobase Publishing. pp. 83–. <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/978-1-4381-0968-8" title="Специјална:ПечатенИзвор/978-1-4381-0968-8">978-1-4381-0968-8</a>.</span> </li> <li id="cite_note-15"><span class="mw-cite-backlink"><a href="#cite_ref-15">↑</a></span> <span class="reference-text">Clare P. Marshall, Rhodes W. Fairbridge (1999) <i>Encyclopedia of Geochemistry</i>, Kluwer Academic Publishers <a href="/wiki/ISBN_(identifier)" class="mw-redirect" title="ISBN (identifier)">ISBN</a> <a href="/wiki/%D0%A1%D0%BF%D0%B5%D1%86%D0%B8%D1%98%D0%B0%D0%BB%D0%BD%D0%B0:%D0%9F%D0%B5%D1%87%D0%B0%D1%82%D0%B5%D0%BD%D0%98%D0%B7%D0%B2%D0%BE%D1%80/0-412-75500-9" title="Специјална:ПечатенИзвор/0-412-75500-9">0-412-75500-9</a></span> </li> <li id="cite_note-PaWh2016-16"><span class="mw-cite-backlink"><a href="#cite_ref-PaWh2016_16-0">↑</a></span> <span class="reference-text"><cite id="CITEREFPalinWhite2016" class="citation journal">Palin, Richard M.; White, Richard W. (2016). <a rel="nofollow" class="external text" href="https://ora.ox.ac.uk/objects/uuid:48630722-57a2-4dd7-8101-92ea1c8df8a1">„Emergence of blueschists on Earth linked to secular changes in oceanic crust composition“</a>. <i>Nature Geoscience</i>. <b>9</b> (1): 60. <a href="/wiki/Bibcode" title="Bibcode">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2016NatGe...9...60P">2016NatGe...9...60P</a>. <a href="/wiki/Doi" class="mw-redirect" title="Doi">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1038%2Fngeo2605">10.1038/ngeo2605</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Nature+Geoscience&rft.atitle=Emergence+of+blueschists+on+Earth+linked+to+secular+changes+in+oceanic+crust+composition&rft.volume=9&rft.issue=1&rft.pages=60&rft.date=2016&rft_id=info%3Adoi%2F10.1038%2Fngeo2605&rft_id=info%3Abibcode%2F2016NatGe...9...60P&rft.aulast=Palin&rft.aufirst=Richard+M.&rft.au=White%2C+Richard+W.&rft_id=https%3A%2F%2Fora.ox.ac.uk%2Fobjects%2Fuuid%3A48630722-57a2-4dd7-8101-92ea1c8df8a1&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-17"><span class="mw-cite-backlink"><a href="#cite_ref-17">↑</a></span> <span class="reference-text"><cite class="citation web"><a rel="nofollow" class="external text" href="https://pubs.usgs.gov/gip/dynamic/understanding.html">„Understanding plate motions [This Dynamic Earth, USGS]“</a>. <i>pubs.usgs.gov</i><span class="reference-accessdate">. Посетено на <span class="nowrap">2017-04-16</span></span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=unknown&rft.jtitle=pubs.usgs.gov&rft.atitle=Understanding+plate+motions+%5BThis+Dynamic+Earth%2C+USGS%5D&rft_id=https%3A%2F%2Fpubs.usgs.gov%2Fgip%2Fdynamic%2Funderstanding.html&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-18"><span class="mw-cite-backlink"><a href="#cite_ref-18">↑</a></span> <span class="reference-text"><cite id="CITEREFMcKenzieJacksonPriestley2005" class="citation journal">McKenzie, Dan; Jackson, James; Priestley, Keith (May 2005). „Thermal structure of oceanic and continental lithosphere“. <i>Earth and Planetary Science Letters</i>. <b>233</b> (3–4): 337–349. <a href="/wiki/Doi" class="mw-redirect" title="Doi">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1016%2Fj.epsl.2005.02.005">10.1016/j.epsl.2005.02.005</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Earth+and+Planetary+Science+Letters&rft.atitle=Thermal+structure+of+oceanic+and+continental+lithosphere&rft.volume=233&rft.issue=3%E2%80%934&rft.pages=337-349&rft.date=2005-05&rft_id=info%3Adoi%2F10.1016%2Fj.epsl.2005.02.005&rft.aulast=McKenzie&rft.aufirst=Dan&rft.au=Jackson%2C+James&rft.au=Priestley%2C+Keith&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-19"><span class="mw-cite-backlink"><a href="#cite_ref-19">↑</a></span> <span class="reference-text">Condie, K.C. 1997. Plate Tectonics and Crustal Evolution (4th Edition). 288 page, Butterworth-Heinemann Ltd.</span> </li> <li id="cite_note-20"><span class="mw-cite-backlink"><a href="#cite_ref-20">↑</a></span> <span class="reference-text"><cite id="CITEREFMüller2008" class="citation journal">Müller, R. Dietmar (April 2008). <a rel="nofollow" class="external text" href="https://www.newscientist.com/article/2100988-worlds-oldest-ocean-crust-dates-back-to-ancient-supercontinent/">„Age, spreading rates, and spreading asymmetry of the world's ocean crust“</a>. <i>Geochemistry, Geophysics, Geosystems</i>. <b>9</b> (4): Q04006. <a href="/wiki/Bibcode" title="Bibcode">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/2008GGG.....9.4006M">2008GGG.....9.4006M</a>. <a href="/wiki/Doi" class="mw-redirect" title="Doi">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1029%2F2007GC001743">10.1029/2007GC001743</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Geochemistry%2C+Geophysics%2C+Geosystems&rft.atitle=Age%2C+spreading+rates%2C+and+spreading+asymmetry+of+the+world%27s+ocean+crust&rft.volume=9&rft.issue=4&rft.pages=Q04006&rft.date=2008-04&rft_id=info%3Adoi%2F10.1029%2F2007GC001743&rft_id=info%3Abibcode%2F2008GGG.....9.4006M&rft.aulast=M%C3%BCller&rft.aufirst=R.+Dietmar&rft_id=https%3A%2F%2Fwww.newscientist.com%2Farticle%2F2100988-worlds-oldest-ocean-crust-dates-back-to-ancient-supercontinent%2F&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-21"><span class="mw-cite-backlink"><a href="#cite_ref-21">↑</a></span> <span class="reference-text"><cite id="CITEREFBenson2016" class="citation web">Benson, Emily (15 August 2016). <a rel="nofollow" class="external text" href="https://www.newscientist.com/article/2100988-worlds-oldest-ocean-crust-dates-back-to-ancient-supercontinent/">„World's oldest ocean crust dates back to ancient supercontinent“</a>. <i>www.newscientist.com</i>. New Scientist<span class="reference-accessdate">. Посетено на <span class="nowrap">11 September</span> 2016</span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=unknown&rft.jtitle=www.newscientist.com&rft.atitle=World%27s+oldest+ocean+crust+dates+back+to+ancient+supercontinent&rft.date=2016-08-15&rft.aulast=Benson&rft.aufirst=Emily&rft_id=https%3A%2F%2Fwww.newscientist.com%2Farticle%2F2100988-worlds-oldest-ocean-crust-dates-back-to-ancient-supercontinent%2F&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-22"><span class="mw-cite-backlink"><a href="#cite_ref-22">↑</a></span> <span class="reference-text"><cite class="citation web"><a rel="nofollow" class="external text" href="https://www.sciencedaily.com/releases/2016/08/160815114933.htm">„Researcher uncovers 340 million year-old oceanic crust in the Mediterranean Sea using magnetic data“</a>. <i>www.sciencedaily.com</i>. <a href="/w/index.php?title=Science_Daily&action=edit&redlink=1" class="new" title="Science Daily (страницата не постои)">Science Daily</a>. 15 August 2016<span class="reference-accessdate">. Посетено на <span class="nowrap">11 September</span> 2016</span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=unknown&rft.jtitle=www.sciencedaily.com&rft.atitle=Researcher+uncovers+340+million+year-old+oceanic+crust+in+the+Mediterranean+Sea+using+magnetic+data&rft.date=2016-08-15&rft_id=https%3A%2F%2Fwww.sciencedaily.com%2Freleases%2F2016%2F08%2F160815114933.htm&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> <li id="cite_note-23"><span class="mw-cite-backlink"><a href="#cite_ref-23">↑</a></span> <span class="reference-text"><cite id="CITEREFPitmanHerronHeirtzler1968" class="citation journal">Pitman, W. C.; Herron, E. M.; Heirtzler, J. R. (1968-03-15). „Magnetic anomalies in the Pacific and sea floor spreading“. <i>Journal of Geophysical Research</i> (англиски). <b>73</b> (6): 2069–2085. <a href="/wiki/Bibcode" title="Bibcode">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1968JGR....73.2069P">1968JGR....73.2069P</a>. <a href="/wiki/Doi" class="mw-redirect" title="Doi">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1029%2FJB073i006p02069">10.1029/JB073i006p02069</a>. <a href="/wiki/ISSN" title="ISSN">ISSN</a> <a rel="nofollow" class="external text" href="//www.worldcat.org/issn/2156-2202">2156-2202</a>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.jtitle=Journal+of+Geophysical+Research&rft.atitle=Magnetic+anomalies+in+the+Pacific+and+sea+floor+spreading&rft.volume=73&rft.issue=6&rft.pages=2069-2085&rft.date=1968-03-15&rft.issn=2156-2202&rft_id=info%3Adoi%2F10.1029%2FJB073i006p02069&rft_id=info%3Abibcode%2F1968JGR....73.2069P&rft.aulast=Pitman&rft.aufirst=W.+C.&rft.au=Herron%2C+E.+M.&rft.au=Heirtzler%2C+J.+R.&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></span> </li> </ol></div></div> <div class="mw-heading mw-heading2"><h2 id="Надворешни_врски"><span id=".D0.9D.D0.B0.D0.B4.D0.B2.D0.BE.D1.80.D0.B5.D1.88.D0.BD.D0.B8_.D0.B2.D1.80.D1.81.D0.BA.D0.B8"></span>Надворешни врски</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&veaction=edit&section=6" title="Уреди го одделот „Надворешни врски“" class="mw-editsection-visualeditor"><span>уреди</span></a><span class="mw-editsection-divider"> | </span><a href="/w/index.php?title=%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0&action=edit&section=6" title="Уреди изворен код на одделот: Надворешни врски"><span>уреди извор</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li><cite id="CITEREFMarshak2005" class="citation book">Marshak, Stephen (2005). <i>Earth: Portrait of a Planet</i>. стр. 41–87.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=book&rft.btitle=Earth%3A+Portrait+of+a+Planet&rft.pages=41-87&rft.date=2005&rft.aulast=Marshak&rft.aufirst=Stephen&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></li> <li><cite id="CITEREFMcDuffHeath" class="citation web">McDuff, Russell E.; Heath, G. Ross. <a rel="nofollow" class="external text" href="http://www2.ocean.washington.edu/oc540/lec01-1/">„Ocean 540: Oceanic Lithosphere; Plate Tectonics; Seafloor Topography“</a>. School of Oceanography, University of Washington<span class="reference-accessdate">. Посетено на <span class="nowrap">9 August</span> 2009</span>.</cite><span title="ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Abook&rft.genre=unknown&rft.btitle=Ocean+540%3A+Oceanic+Lithosphere%3B+Plate+Tectonics%3B+Seafloor+Topography&rft.pub=School+of+Oceanography%2C+University+of+Washington&rft.aulast=McDuff&rft.aufirst=Russell+E.&rft.au=Heath%2C+G.+Ross&rft_id=http%3A%2F%2Fwww2.ocean.washington.edu%2Foc540%2Flec01-1%2F&rfr_id=info%3Asid%2Fmk.wikipedia.org%3A%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0+%D0%BA%D0%BE%D1%80%D0%B0" class="Z3988"></span><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r5289462"></li></ul> <table class="navbox" style="border-spacing:0"><tbody><tr><td style="padding:2px"><table class="nowraplinks hlist collapsible autocollapse navbox-inner" style="border-spacing:0;background:transparent;color:inherit"><tbody><tr><th scope="col" class="navbox-title" colspan="3"><div class="plainlinks hlist navbar mini"><ul><li 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href="https://mk.wikipedia.org/w/index.php?title=%D0%9F%D1%80%D0%B5%D0%B4%D0%BB%D0%BE%D1%88%D0%BA%D0%B0:%D0%A4%D0%B8%D0%B7%D0%B8%D1%87%D0%BA%D0%B0_%D0%BE%D0%BA%D0%B5%D0%B0%D0%BD%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0&action=edit"><abbr title="Уредување на предлошкава" style=";;background:none transparent;border:none;">у</abbr></a></li></ul></div><div style="font-size:110%"><a href="/wiki/%D0%A4%D0%B8%D0%B7%D0%B8%D1%87%D0%BA%D0%B0_%D0%BE%D0%BA%D0%B5%D0%B0%D0%BD%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0" title="Физичка океанографија">Физичка океанографија</a></div></th></tr><tr style="height:2px"><td colspan="2"></td></tr><tr><th scope="row" class="navbox-group"><a href="/wiki/%D0%91%D1%80%D0%B0%D0%BD" title="Бран">Бранови</a></th><td class="navbox-list navbox-odd" style="text-align:left;border-left-width:2px;border-left-style:solid;width:100%;padding:0px"><div style="padding:0em 0.25em"> <ul><li><a href="/wiki/%D0%95%D1%98%D1%80%D0%BE%D0%B2%D0%B0_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B0_%D1%82%D0%B5%D0%BE%D1%80%D0%B8%D1%98%D0%B0" title="Ејрова бранова теорија">Ејрова бранова теорија</a></li> <li><a href="/w/index.php?title=%D0%91%D0%B0%D0%BB%D0%B0%D0%BD%D1%82%D0%B0%D1%98%D0%BD%D0%BE%D0%B2%D0%B0_%D1%81%D0%BA%D0%B0%D0%BB%D0%B0&action=edit&redlink=1" class="new" title="Балантајнова скала (страницата не постои)">Балантајнова скала</a></li> <li><a href="/w/index.php?title=%D0%91%D0%B5%D0%BD%D1%9F%D0%B0%D0%BC%D0%B8%D0%BD%E2%80%93%D0%A4%D0%B5%D1%98%D1%80%D0%BE%D0%B2%D0%B0_%D0%BD%D0%B5%D1%81%D1%82%D0%B0%D0%B1%D0%B8%D0%BB%D0%BD%D0%BE%D1%81%D1%82&action=edit&redlink=1" class="new" title="Бенџамин–Фејрова нестабилност (страницата не постои)">Бенџамин–Фејрова нестабилност</a></li> <li><a href="/w/index.php?title=%D0%91%D1%83%D1%81%D0%B8%D0%BD%D0%B5%D1%81%D0%BA%D0%BE%D0%B2%D0%B0_%D0%B0%D0%BF%D1%80%D0%BE%D0%BA%D1%81%D0%B8%D0%BC%D0%B0%D1%86%D0%B8%D1%98%D0%B0&action=edit&redlink=1" class="new" title="Бусинескова апроксимација (страницата не постои)">Бусинескова апроксимација</a></li> <li><a href="/w/index.php?title=%D0%9F%D1%80%D0%B5%D0%BB%D0%BE%D0%BC%D0%BD%D0%B8%D0%BA&action=edit&redlink=1" class="new" title="Преломник (страницата не постои)">Преломник</a></li> <li><a href="/w/index.php?title=%D0%9A%D0%BB%D0%B0%D0%BF%D0%BE%D1%82%D0%B8%D1%81&action=edit&redlink=1" class="new" title="Клапотис (страницата не постои)">Клапотис</a></li> <li><a href="/wiki/%D0%9A%D0%BD%D0%BE%D0%B8%D0%B4%D0%B0%D0%BB%D0%B5%D0%BD_%D0%B1%D1%80%D0%B0%D0%BD" title="Кноидален бран">Кноидален бран</a></li> <li><a href="/w/index.php?title=%D0%9D%D0%B0%D0%BA%D1%80%D1%81%D0%BD%D0%BE_%D0%BC%D0%BE%D1%80%D0%B5&action=edit&redlink=1" class="new" title="Накрсно море (страницата не постои)">Накрсно море</a></li> <li><a href="/w/index.php?title=%D0%A0%D0%B0%D1%81%D0%B5%D1%98%D1%83%D0%B2%D0%B0%D1%9A%D0%B5_(%D0%B2%D0%BE%D0%B4%D0%B5%D0%BD%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8)&action=edit&redlink=1" class="new" title="Расејување (водени бранови) (страницата не постои)">Расејување</a></li> <li><a href="/w/index.php?title=%D0%98%D0%BD%D1%84%D0%B0%D0%B3%D1%80%D0%B0%D0%B2%D0%B8%D1%82%D0%B0%D1%86%D0%B8%D0%BE%D0%BD%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8&action=edit&redlink=1" class="new" title="Инфагравитациони бранови (страницата не постои)">Инфагравитациони бранови</a></li> <li><a href="/w/index.php?title=%D0%9A%D1%80%D0%B0%D1%98%D0%B1%D1%80%D0%B5%D0%B6%D0%BD%D0%B8_%D0%BA%D0%BE%D0%BF%D0%BD%D0%B5%D0%BD%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8&action=edit&redlink=1" class="new" title="Крајбрежни копнени бранови (страницата не постои)">Крајбрежни копнени бранови</a></li> <li><a href="/wiki/%D0%95%D0%BA%D0%B2%D0%B0%D1%82%D0%BE%D1%80%D1%81%D0%BA%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8" title="Екваторски бранови">Екваторски бранови</a></li> <li><a href="/w/index.php?title=%D0%9F%D0%BE%D0%B2%D1%82%D0%BE%D1%80%D0%BB%D0%B8%D0%B2%D0%BE%D1%81%D1%82_(%D0%B3%D0%B5%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0)&action=edit&redlink=1" class="new" title="Повторливост (географија) (страницата не постои)">Повторливост</a></li> <li><a href="/w/index.php?title=%D0%A2%D0%B5%D0%B6%D0%B8%D0%BD%D1%81%D0%BA%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8&action=edit&redlink=1" class="new" title="Тежински бранови (страницата не постои)">Тежински бранови</a></li> <li><a href="/w/index.php?title=%D0%92%D0%BD%D0%B0%D1%82%D1%80%D0%B5%D1%88%D0%BD%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8&action=edit&redlink=1" class="new" title="Внатрешни бранови (страницата не постои)">Внатрешни бранови</a></li> <li><a href="/wiki/%D0%9A%D0%B5%D0%BB%D0%B2%D0%B8%D0%BD%D0%BE%D0%B2_%D0%B1%D1%80%D0%B0%D0%BD" title="Келвинов бран">Келвинов бран</a></li> <li><a href="/w/index.php?title=%D0%9A%D0%B8%D0%BD%D0%B5%D0%BC%D0%B0%D1%82%D0%B8%D1%87%D0%BA%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD&action=edit&redlink=1" class="new" title="Кинематички бран (страницата не постои)">Кинематички бран</a></li> <li><a href="/w/index.php?title=%D0%9A%D1%80%D0%B0%D1%98%D0%B1%D1%80%D0%B5%D0%B6%D0%B5%D0%BD_%D0%BD%D0%B0%D0%BD%D0%BE%D1%81&action=edit&redlink=1" class="new" title="Крајбрежен нанос (страницата не постои)">Крајбрежен нанос</a></li> <li><a href="/w/index.php?title=%D0%9B%D1%83%D0%BA%D0%BE%D0%B2_%D0%BF%D1%80%D0%B8%D0%BD%D1%86%D0%B8%D0%BF_%D0%BD%D0%B0_%D0%BF%D1%80%D0%BE%D0%BC%D0%B5%D0%BD%D0%BB%D0%B2%D0%B8%D0%BE%D1%81%D1%82&action=edit&redlink=1" class="new" title="Луков принцип на променлвиост (страницата не постои)">Луков принцип на променлвиост</a></li> <li><a href="/w/index.php?title=%D0%A0%D0%B0%D0%B2%D0%B5%D0%BD%D0%BA%D0%B0_%D0%BD%D0%B0_%D0%B1%D0%BB%D0%B0%D0%B3%D0%B0_%D0%BD%D0%B0%D0%BA%D0%BE%D1%81%D0%B5%D0%BD%D0%BE%D1%81%D1%82&action=edit&redlink=1" class="new" title="Равенка на блага накосеност (страницата не постои)">Равенка на блага накосеност</a></li> <li><a href="/w/index.php?title=%D0%A1%D1%82%D1%80%D0%B5%D1%81_%D0%BD%D0%B0_%D0%BF%D1%80%D0%BE%D1%82%D0%B5%D0%B3%D0%B0%D1%9A%D0%B5&action=edit&redlink=1" class="new" title="Стрес на протегање (страницата не постои)">Стрес на протегање</a></li> <li><a href="/w/index.php?title=%D0%A3%D0%B1%D0%B8%D1%81%D1%82%D0%B2%D0%B5%D0%BD_%D0%B1%D1%80%D0%B0%D0%BD&action=edit&redlink=1" class="new" title="Убиствен бран (страницата не постои)">Убиствен бран</a></li> <li><a href="/w/index.php?title=%D0%A0%D0%BE%D1%81%D0%B1%D0%B8%D0%B5%D0%B2_%D0%B1%D1%80%D0%B0%D0%BD&action=edit&redlink=1" class="new" title="Росбиев бран (страницата не постои)">Росбиев бран</a></li> <li><a href="/w/index.php?title=%D0%A0%D0%BE%D1%81%D0%B1%D0%B8%D0%B5%D0%B2%D0%B8_%D1%82%D0%B5%D0%B6%D0%B8%D0%BD%D1%81%D0%BA%D0%B8_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%B8&action=edit&redlink=1" class="new" title="Росбиеви тежински бранови 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href="/w/index.php?title=%D0%A1%D1%82%D0%BE%D0%BA%D1%81%D0%BE%D0%B2%D0%B0_%D0%B3%D1%80%D0%B0%D0%BD%D0%B8%D1%87%D0%BD%D0%B0_%D0%BE%D0%B1%D0%B2%D0%B8%D0%B2%D0%BA%D0%B0&action=edit&redlink=1" class="new" title="Стоксова гранична обвивка (страницата не постои)">Стоксова гранична обвивка</a></li> <li><a href="/w/index.php?title=%D0%A1%D1%82%D0%BE%D0%BA%D1%81%D0%BE%D0%B2%D0%BE_%D0%BF%D0%BB%D0%BE%D0%B2%D0%B5%D1%9A%D0%B5&action=edit&redlink=1" class="new" title="Стоксово пловење (страницата не постои)">Стоксово пловење</a></li> <li><a href="/w/index.php?title=%D0%A1%D1%82%D0%BE%D0%BA%D1%81%D0%BE%D0%B2_%D0%B1%D1%80%D0%B0%D0%BD&action=edit&redlink=1" class="new" title="Стоксов бран (страницата не постои)">Стоксов бран</a></li> <li><a href="/wiki/%D0%A1%D1%83%D1%80%D1%84%D0%B0%D1%9A%D0%B5" title="Сурфање">Сурфање</a></li> <li><a href="/w/index.php?title=%D0%9D%D0%B0%D0%B4%D1%83%D0%B5%D0%BD%D0%BE%D1%81%D1%82_(%D0%BE%D0%BA%D0%B5%D0%B0%D0%BD)&action=edit&redlink=1" class="new" title="Надуеност 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href="/w/index.php?title=%D0%9E%D1%81%D0%BD%D0%BE%D0%B2%D0%B0_%D0%BD%D0%B0_%D0%B1%D1%80%D0%B0%D0%BD%D0%BE%D1%82&action=edit&redlink=1" class="new" title="Основа на бранот (страницата не постои)">Основа на бранот</a></li> <li><a href="/w/index.php?title=%D0%91%D1%80%D0%B0%D0%BD%D0%BE%D0%B2%D0%BE-%D1%81%D1%82%D1%80%D1%83%D1%98%D0%BD%D0%BE_%D0%B7%D0%B0%D0%B5%D0%BC%D0%BE%D0%B4%D0%B5%D1%98%D1%81%D1%82%D0%B2%D0%BE&action=edit&redlink=1" class="new" title="Браново-струјно заемодејство (страницата не постои)">Браново-струјно заемодејство</a></li> <li><a href="/w/index.php?title=%D0%92%D0%B8%D1%81%D0%B8%D0%BD%D0%B0_%D0%BD%D0%B0_%D0%B1%D1%80%D0%B0%D0%BD&action=edit&redlink=1" class="new" title="Висина на бран (страницата не постои)">Висина на бран</a></li> <li><a href="/w/index.php?title=%D0%9C%D0%BE%D1%9C%D0%BD%D0%BE%D1%81%D1%82_%D0%BD%D0%B0_%D0%B1%D1%80%D0%B0%D0%BD&action=edit&redlink=1" class="new" title="Моќност на бран (страницата не постои)">Моќност на бран</a></li> <li><a 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title="Правило на дванаесетки (страницата не постои)">Правило на дванаесетки</a></li> <li><a href="/wiki/%D0%9C%D1%80%D1%82%D0%B2%D0%B0_%D0%B2%D0%BE%D0%B4%D0%B0" title="Мртва вода">Мртва вода</a></li> <li><a href="/w/index.php?title=%D0%92%D0%B8%D1%81%D0%BE%D0%BA%D0%B8_%D0%BF%D0%BB%D0%B8%D0%BC%D0%B8&action=edit&redlink=1" class="new" title="Високи плими (страницата не постои)">Високи/ниски плими</a></li> <li><a href="/w/index.php?title=%D0%9F%D1%80%D0%B2%D0%B8%D1%87%D0%BD%D0%B0_%D0%BF%D0%BB%D0%B8%D0%BC%D0%B0&action=edit&redlink=1" class="new" title="Првична плима (страницата не постои)">Првична плима</a></li> <li><a href="/wiki/%D0%9F%D0%BB%D0%B8%D0%BC%D0%BD%D0%B0_%D1%81%D0%B8%D0%BB%D0%B0" title="Плимна сила">Плимна сила</a></li> <li><a href="/w/index.php?title=%D0%9F%D0%BB%D0%B8%D0%BC%D0%BD%D0%B0_%D0%BC%D0%BE%D1%9C%D0%BD%D0%BE%D1%81%D1%82&action=edit&redlink=1" class="new" title="Плимна моќност (страницата не постои)">Плимна моќност</a></li> <li><a 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href="/wiki/%D0%9F%D0%BB%D0%B8%D0%BC%D0%BE%D0%BC%D0%B5%D1%80" title="Плимомер">Плимомер</a></li> <li><a href="/wiki/%D0%9A%D0%B0%D1%82%D0%B5%D0%B3%D0%BE%D1%80%D0%B8%D1%98%D0%B0:%D0%9F%D0%BB%D0%B8%D0%BC%D0%B0_%D0%B8_%D0%BE%D1%81%D0%B5%D0%BA%D0%B0" title="Категорија:Плима и осека">Повеќе...</a></li></ul> </div></td></tr><tr style="height:2px"><td colspan="2"></td></tr><tr><th scope="row" class="navbox-group"><a href="/wiki/%D0%97%D0%B5%D0%BC%D1%98%D0%B8%D1%88%D1%82%D0%B5%D0%BD_%D0%BE%D0%B1%D0%BB%D0%B8%D0%BA" title="Земјиштен облик">Земјишни облици</a></th><td class="navbox-list navbox-even" style="text-align:left;border-left-width:2px;border-left-style:solid;width:100%;padding:0px"><div style="padding:0em 0.25em"> <ul><li><a href="/w/index.php?title=%D0%9F%D0%BE%D0%B4%D0%B2%D0%BE%D0%B4%D0%BD%D0%B8_%D0%B4%D0%B5%D0%BB%D1%82%D0%B8&action=edit&redlink=1" class="new" title="Подводни делти (страницата не постои)">Подводни делти</a></li> <li><a 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href="/wiki/%D0%9A%D0%BE%D0%BD%D1%82%D0%B8%D0%BD%D0%B5%D0%BD%D1%82%D0%B0%D0%BB%D0%B5%D0%BD_%D0%BF%D1%80%D0%B0%D0%B3" title="Континентален праг">Континентален праг</a></li> <li><a href="/w/index.php?title=%D0%9A%D0%BE%D0%BD%D1%82%D1%83%D1%80%D0%B8&action=edit&redlink=1" class="new" title="Контури (страницата не постои)">Контури</a></li> <li><a href="/wiki/%D0%A5%D0%B8%D0%B4%D1%80%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0" title="Хидрографија">Хидрографија</a></li> <li><a href="/wiki/%D0%93%D0%B0%D1%98%D0%BE%D1%82" title="Гајот">Гајот</a></li> <li><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%BA%D0%BE%D1%82%D0%BB%D0%B8%D0%BD%D0%B0" class="mw-redirect" title="Океанска котлина">Океанска котлина</a></li> <li><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%B2%D0%B8%D1%81%D0%BE%D1%80%D0%B0%D0%BC%D0%BD%D0%B8%D0%BD%D0%B0" title="Океанска висорамнина">Океанска висорамнина</a></li> <li><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B8_%D1%80%D0%B0%D1%81%D0%B5%D0%B4" class="mw-redirect" title="Океански расед">Океански расед</a></li> <li><a href="/wiki/%D0%9F%D0%B0%D1%81%D0%B8%D0%B2%D0%BD%D0%B0_%D0%B3%D1%80%D0%B0%D0%BD%D0%B8%D1%86%D0%B0" title="Пасивна граница">Пасивна граница</a></li> <li><a href="/wiki/%D0%9C%D0%BE%D1%80%D1%81%D0%BA%D0%BE_%D0%B4%D0%BD%D0%BE" class="mw-redirect" title="Морско дно">Морско дно</a></li> <li><a href="/wiki/%D0%9F%D0%BE%D0%B4%D0%B2%D0%BE%D0%B4%D0%BD%D0%B0_%D0%BF%D0%BB%D0%B0%D0%BD%D0%B8%D0%BD%D0%B0" title="Подводна планина">Подводна планина</a></li> <li><a href="/wiki/%D0%9F%D0%BE%D0%B4%D0%B2%D0%BE%D0%B4%D0%BD%D0%B8_%D0%BA%D0%BB%D0%B8%D1%81%D1%83%D1%80%D0%B8" class="mw-redirect" title="Подводни клисури">Подводни клисури</a></li> <li><a href="/wiki/%D0%9A%D1%80%D0%B0%D1%98%D0%B1%D1%80%D0%B5%D0%B6%D0%BD%D0%B0_%D0%B3%D0%B5%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0" title="Крајбрежна географија">Крајбрежна географија</a></li> 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title="Осветлена зона">Осветлена</a></li> <li><a href="/wiki/%D0%A1%D1%83%D1%80%D1%84%D0%B5%D1%80%D1%81%D0%BA%D0%B0_%D0%B7%D0%BE%D0%BD%D0%B0" title="Сурферска зона">Сурферска зона</a></li></ul> </div></td></tr><tr style="height:2px"><td colspan="2"></td></tr><tr><th scope="row" class="navbox-group"><a href="/wiki/%D0%9C%D0%BE%D1%80%D1%81%D0%BA%D0%BE_%D0%BD%D0%B8%D0%B2%D0%BE" title="Морско ниво">Морско ниво</a></th><td class="navbox-list navbox-odd" style="text-align:left;border-left-width:2px;border-left-style:solid;width:100%;padding:0px"><div style="padding:0em 0.25em"> <ul><li><a href="/wiki/%D0%9C%D0%BE%D0%BC%D0%B5%D0%BD%D1%82%D0%B0%D0%BB%D0%B5%D0%BD_%D1%80%D0%B0%D1%81%D1%82_%D0%BD%D0%B0_%D0%BC%D0%BE%D1%80%D1%81%D0%BA%D0%BE%D1%82%D0%BE_%D0%BD%D0%B8%D0%B2%D0%BE" class="mw-redirect" title="Моментален раст на морското ниво">Моментален раст на морското ниво</a></li> <li><a href="/wiki/%D0%9F%D0%BE%D0%BA%D0%B0%D1%87%D1%83%D0%B2%D0%B0%D1%9A%D0%B5_%D0%BD%D0%B0_%D0%BC%D0%BE%D1%80%D1%81%D0%BA%D0%BE%D1%82%D0%BE_%D0%BD%D0%B8%D0%B2%D0%BE" title="Покачување на морското ниво">Идно морско ниво</a></li> <li><a href="/wiki/%D0%9A%D1%80%D0%B8%D0%B2%D0%B0_%D0%BD%D0%B0_%D0%BC%D0%BE%D1%80%D1%81%D0%BA%D0%BE%D1%82%D0%BE_%D0%BD%D0%B8%D0%B2%D0%BE" title="Крива на морското ниво">Крива на морското ниво</a></li></ul> </div></td></tr><tr style="height:2px"><td colspan="2"></td></tr><tr><th scope="row" class="navbox-group"><a href="/w/index.php?title=%D0%97%D0%B2%D1%83%D1%87%D0%BD%D0%B0_%D0%BE%D0%BA%D0%B5%D0%B0%D0%BD%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0&action=edit&redlink=1" class="new" title="Звучна океанографија (страницата не постои)">Звук</a></th><td class="navbox-list navbox-even" style="text-align:left;border-left-width:2px;border-left-style:solid;width:100%;padding:0px"><div style="padding:0em 0.25em"> <ul><li><a href="/wiki/%D0%9E%D0%BA%D0%B5%D0%B0%D0%BD%D1%81%D0%BA%D0%B0_%D0%B7%D0%B2%D1%83%D1%87%D0%BD%D0%B0_%D1%82%D0%BE%D0%BC%D0%BE%D0%B3%D1%80%D0%B0%D1%84%D0%B8%D1%98%D0%B0" title="Океанска звучна томографија">Океанска звучна томографија</a></li> <li><a href="/wiki/%D0%97%D0%B2%D1%83%D1%87%D0%BD%D0%B0_%D0%B1%D0%BE%D0%BC%D0%B1%D0%B0" title="Звучна бомба">Звучна бомба</a></li> <li><a href="/w/index.php?title=%D0%97%D0%B2%D1%83%D1%87%D0%B5%D0%BD_%D0%BA%D0%B0%D0%BD%D0%B0%D0%BB&action=edit&redlink=1" class="new" title="Звучен канал (страницата не постои)">Звучен канал</a></li> <li><a href="/wiki/%D0%97%D0%B2%D1%83%D0%BA_%D0%B2%D0%BE_%D0%B2%D0%BE%D0%B4%D0%B0" class="mw-redirect" title="Звук во вода">Звук во вода</a></li> <li><a href="/wiki/%D0%A5%D0%B8%D0%B4%D1%80%D0%BE%D0%B0%D0%BA%D1%83%D1%81%D1%82%D0%B8%D0%BA%D0%B0" title="Хидроакустика">Хидроакустика</a></li></ul> </div></td></tr><tr style="height:2px"><td colspan="2"></td></tr><tr><th scope="row" class="navbox-group">Останато</th><td 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href="/wiki/%D0%9A%D0%B0%D1%82%D0%B5%D0%B3%D0%BE%D1%80%D0%B8%D1%98%D0%B0:%D0%A2%D0%B5%D0%BA%D1%82%D0%BE%D0%BD%D0%B8%D0%BA%D0%B0_%D0%BD%D0%B0_%D0%BF%D0%BB%D0%BE%D1%87%D0%B8%D1%82%D0%B5" title="Категорија:Тектоника на плочите">Тектоника на плочите</a></li><li><a href="/wiki/%D0%9A%D0%B0%D1%82%D0%B5%D0%B3%D0%BE%D1%80%D0%B8%D1%98%D0%B0:%D0%97%D0%B5%D0%BC%D1%98%D0%B8%D0%BD%D0%B0_%D0%BA%D0%BE%D1%80%D0%B0" title="Категорија:Земјина кора">Земјина кора</a></li></ul></div><div id="mw-hidden-catlinks" class="mw-hidden-catlinks mw-hidden-cats-hidden">Скриена категорија: <ul><li><a href="/wiki/%D0%9A%D0%B0%D1%82%D0%B5%D0%B3%D0%BE%D1%80%D0%B8%D1%98%D0%B0:%D0%A1%D1%82%D0%B0%D1%82%D0%B8%D0%B8_%D1%81%D0%BE_%D0%B8%D0%B7%D0%B2%D0%BE%D1%80%D0%B8_%D0%BD%D0%B0_%D0%B0%D0%BD%D0%B3%D0%BB%D0%B8%D1%81%D0%BA%D0%B8_(en)" title="Категорија:Статии со извори на англиски (en)">Статии со извори на англиски (en)</a></li></ul></div></div> </div> </main> </div> <div class="mw-footer-container"> <footer id="footer" 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