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Rift - Wikipedia

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class="vector-toc-numb">2</span> <span>Rift development</span> </div> </a> <button aria-controls="toc-Rift_development-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Toggle Rift development subsection</span> </button> <ul id="toc-Rift_development-sublist" class="vector-toc-list"> <li id="toc-Rift_initiation" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Rift_initiation"> <div class="vector-toc-text"> <span class="vector-toc-numb">2.1</span> <span>Rift initiation</span> </div> </a> <ul id="toc-Rift_initiation-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Mature_rift_stage" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Mature_rift_stage"> <div class="vector-toc-text"> <span class="vector-toc-numb">2.2</span> <span>Mature rift stage</span> </div> </a> <ul id="toc-Mature_rift_stage-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Post-rift_subsidence" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Post-rift_subsidence"> <div class="vector-toc-text"> <span class="vector-toc-numb">2.3</span> <span>Post-rift subsidence</span> </div> </a> <ul id="toc-Post-rift_subsidence-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Multiphase_rifting" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Multiphase_rifting"> <div class="vector-toc-text"> <span class="vector-toc-numb">2.4</span> <span>Multiphase rifting</span> </div> </a> <ul id="toc-Multiphase_rifting-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Rifting_to_break-up" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Rifting_to_break-up"> <div class="vector-toc-text"> <span class="vector-toc-numb">2.5</span> <span>Rifting to break-up</span> </div> </a> <ul id="toc-Rifting_to_break-up-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Magmatism" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Magmatism"> <div class="vector-toc-text"> <span class="vector-toc-numb">3</span> <span>Magmatism</span> </div> </a> <ul id="toc-Magmatism-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Economic_importance" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Economic_importance"> <div class="vector-toc-text"> <span class="vector-toc-numb">4</span> <span>Economic importance</span> </div> </a> <button aria-controls="toc-Economic_importance-sublist" class="cdx-button cdx-button--weight-quiet cdx-button--icon-only vector-toc-toggle"> <span class="vector-icon mw-ui-icon-wikimedia-expand"></span> <span>Toggle Economic importance subsection</span> </button> <ul id="toc-Economic_importance-sublist" class="vector-toc-list"> <li id="toc-Mineral_deposits" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Mineral_deposits"> <div class="vector-toc-text"> <span class="vector-toc-numb">4.1</span> <span>Mineral deposits</span> </div> </a> <ul id="toc-Mineral_deposits-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Oil_and_gas" class="vector-toc-list-item vector-toc-level-2"> <a class="vector-toc-link" href="#Oil_and_gas"> <div class="vector-toc-text"> <span class="vector-toc-numb">4.2</span> <span>Oil and gas</span> </div> </a> <ul id="toc-Oil_and_gas-sublist" class="vector-toc-list"> </ul> </li> </ul> </li> <li id="toc-Examples" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Examples"> <div class="vector-toc-text"> <span class="vector-toc-numb">5</span> <span>Examples</span> </div> </a> <ul id="toc-Examples-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-See_also" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#See_also"> <div class="vector-toc-text"> <span class="vector-toc-numb">6</span> <span>See also</span> </div> </a> <ul id="toc-See_also-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-References" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#References"> <div class="vector-toc-text"> <span class="vector-toc-numb">7</span> <span>References</span> </div> </a> <ul id="toc-References-sublist" class="vector-toc-list"> </ul> </li> <li id="toc-Further_reading" class="vector-toc-list-item vector-toc-level-1 vector-toc-list-item-expanded"> <a class="vector-toc-link" href="#Further_reading"> <div class="vector-toc-text"> <span class="vector-toc-numb">8</span> <span>Further reading</span> </div> </a> <ul id="toc-Further_reading-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="Contents" class="vector-toc-landmark"> <div id="vector-page-titlebar-toc" class="vector-dropdown vector-page-titlebar-toc vector-button-flush-left" title="Table of Contents" > <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="Toggle the table of contents" > <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">Toggle the table of contents</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">Rift</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="Go to an article in another language. Available in 47 languages" > <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-47" 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">47 languages</span> </label> <div class="vector-dropdown-content"> <div class="vector-menu-content"> <ul class="vector-menu-content-list"> <li class="interlanguage-link interwiki-als mw-list-item"><a href="https://als.wikipedia.org/wiki/Grabenbruch" title="Grabenbruch – Alemannic" lang="gsw" hreflang="gsw" data-title="Grabenbruch" data-language-autonym="Alemannisch" data-language-local-name="Alemannic" class="interlanguage-link-target"><span>Alemannisch</span></a></li><li class="interlanguage-link interwiki-ar mw-list-item"><a href="https://ar.wikipedia.org/wiki/%D8%AE%D8%B3%D9%81_(%D8%AC%D9%8A%D9%88%D9%84%D9%88%D8%AC%D9%8A%D8%A7)" title="خسف (جيولوجيا) – Arabic" lang="ar" hreflang="ar" data-title="خسف (جيولوجيا)" data-language-autonym="العربية" data-language-local-name="Arabic" class="interlanguage-link-target"><span>العربية</span></a></li><li class="interlanguage-link interwiki-ast mw-list-item"><a href="https://ast.wikipedia.org/wiki/Rift" title="Rift – Asturian" lang="ast" hreflang="ast" data-title="Rift" data-language-autonym="Asturianu" data-language-local-name="Asturian" class="interlanguage-link-target"><span>Asturianu</span></a></li><li class="interlanguage-link interwiki-az mw-list-item"><a href="https://az.wikipedia.org/wiki/Rift" title="Rift – Azerbaijani" lang="az" hreflang="az" data-title="Rift" data-language-autonym="Azərbaycanca" data-language-local-name="Azerbaijani" class="interlanguage-link-target"><span>Azərbaycanca</span></a></li><li class="interlanguage-link interwiki-be mw-list-item"><a href="https://be.wikipedia.org/wiki/%D0%A0%D1%8B%D1%84%D1%82" title="Рыфт – Belarusian" lang="be" hreflang="be" data-title="Рыфт" data-language-autonym="Беларуская" data-language-local-name="Belarusian" class="interlanguage-link-target"><span>Беларуская</span></a></li><li class="interlanguage-link interwiki-bh mw-list-item"><a href="https://bh.wikipedia.org/wiki/%E0%A4%B0%E0%A4%BF%E0%A4%AB%E0%A5%8D%E0%A4%9F" title="रिफ्ट – Bhojpuri" lang="bh" hreflang="bh" data-title="रिफ्ट" 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%A0%D0%B8%D1%84%D1%82" title="Рифт – Bulgarian" lang="bg" hreflang="bg" data-title="Рифт" data-language-autonym="Български" data-language-local-name="Bulgarian" 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/Rift" title="Rift – Catalan" lang="ca" hreflang="ca" data-title="Rift" data-language-autonym="Català" data-language-local-name="Catalan" 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/Rift" title="Rift – Czech" lang="cs" hreflang="cs" data-title="Rift" data-language-autonym="Čeština" data-language-local-name="Czech" class="interlanguage-link-target"><span>Čeština</span></a></li><li class="interlanguage-link interwiki-de mw-list-item"><a href="https://de.wikipedia.org/wiki/Grabenbruch" title="Grabenbruch – German" lang="de" hreflang="de" data-title="Grabenbruch" data-language-autonym="Deutsch" data-language-local-name="German" 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/Rift" title="Rift – Estonian" lang="et" hreflang="et" data-title="Rift" data-language-autonym="Eesti" data-language-local-name="Estonian" class="interlanguage-link-target"><span>Eesti</span></a></li><li class="interlanguage-link interwiki-es mw-list-item"><a href="https://es.wikipedia.org/wiki/Rift" title="Rift – Spanish" lang="es" hreflang="es" data-title="Rift" data-language-autonym="Español" data-language-local-name="Spanish" 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/Rifto" title="Rifto – Esperanto" lang="eo" hreflang="eo" data-title="Rifto" data-language-autonym="Esperanto" data-language-local-name="Esperanto" 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/Rift_gunea" title="Rift gunea – Basque" lang="eu" hreflang="eu" data-title="Rift gunea" data-language-autonym="Euskara" data-language-local-name="Basque" 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/%DA%A9%D8%A7%D9%81%D8%AA_(%D8%B2%D9%85%DB%8C%D9%86%E2%80%8C%D8%B4%D9%86%D8%A7%D8%B3%DB%8C)" title="کافت (زمین‌شناسی) – Persian" lang="fa" hreflang="fa" data-title="کافت (زمین‌شناسی)" data-language-autonym="فارسی" data-language-local-name="Persian" 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/Rift" title="Rift – French" lang="fr" hreflang="fr" data-title="Rift" data-language-autonym="Français" data-language-local-name="French" class="interlanguage-link-target"><span>Français</span></a></li><li class="interlanguage-link interwiki-gl mw-list-item"><a href="https://gl.wikipedia.org/wiki/Rift" title="Rift – Galician" lang="gl" hreflang="gl" data-title="Rift" data-language-autonym="Galego" data-language-local-name="Galician" 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/%EC%97%B4%EA%B0%9C%EC%A7%80" title="열개지 – Korean" lang="ko" hreflang="ko" data-title="열개지" data-language-autonym="한국어" data-language-local-name="Korean" class="interlanguage-link-target"><span>한국어</span></a></li><li class="interlanguage-link interwiki-hy mw-list-item"><a href="https://hy.wikipedia.org/wiki/%D5%8C%D5%AB%D6%86%D5%BF" title="Ռիֆտ – Armenian" lang="hy" hreflang="hy" data-title="Ռիֆտ" data-language-autonym="Հայերեն" data-language-local-name="Armenian" class="interlanguage-link-target"><span>Հայերեն</span></a></li><li class="interlanguage-link interwiki-hi mw-list-item"><a href="https://hi.wikipedia.org/wiki/%E0%A4%B0%E0%A4%BF%E0%A4%AB%E0%A4%BC%E0%A5%8D%E0%A4%9F_(%E0%A4%AD%E0%A5%82%E0%A4%B5%E0%A4%BF%E0%A4%9C%E0%A5%8D%E0%A4%9E%E0%A4%BE%E0%A4%A8)" title="रिफ़्ट (भूविज्ञान) – Hindi" lang="hi" hreflang="hi" data-title="रिफ़्ट (भूविज्ञान)" data-language-autonym="हिन्दी" data-language-local-name="Hindi" class="interlanguage-link-target"><span>हिन्दी</span></a></li><li class="interlanguage-link interwiki-id mw-list-item"><a href="https://id.wikipedia.org/wiki/Retakan_(geologi)" title="Retakan (geologi) – Indonesian" lang="id" hreflang="id" data-title="Retakan (geologi)" data-language-autonym="Bahasa Indonesia" data-language-local-name="Indonesian" class="interlanguage-link-target"><span>Bahasa Indonesia</span></a></li><li class="interlanguage-link interwiki-it mw-list-item"><a href="https://it.wikipedia.org/wiki/Rift" title="Rift – Italian" lang="it" hreflang="it" data-title="Rift" data-language-autonym="Italiano" data-language-local-name="Italian" class="interlanguage-link-target"><span>Italiano</span></a></li><li class="interlanguage-link interwiki-he mw-list-item"><a href="https://he.wikipedia.org/wiki/%D7%91%D7%A7%D7%A2_(%D7%92%D7%90%D7%95%D7%9C%D7%95%D7%92%D7%99%D7%94)" title="בקע (גאולוגיה) – Hebrew" lang="he" hreflang="he" data-title="בקע (גאולוגיה)" data-language-autonym="עברית" data-language-local-name="Hebrew" class="interlanguage-link-target"><span>עברית</span></a></li><li class="interlanguage-link interwiki-ka mw-list-item"><a href="https://ka.wikipedia.org/wiki/%E1%83%A0%E1%83%98%E1%83%A4%E1%83%A2%E1%83%98" title="რიფტი – Georgian" lang="ka" hreflang="ka" data-title="რიფტი" data-language-autonym="ქართული" data-language-local-name="Georgian" class="interlanguage-link-target"><span>ქართული</span></a></li><li class="interlanguage-link interwiki-kk mw-list-item"><a href="https://kk.wikipedia.org/wiki/%D0%A0%D0%B8%D1%84%D1%82" title="Рифт – Kazakh" lang="kk" hreflang="kk" data-title="Рифт" data-language-autonym="Қазақша" data-language-local-name="Kazakh" class="interlanguage-link-target"><span>Қазақша</span></a></li><li class="interlanguage-link interwiki-sw mw-list-item"><a href="https://sw.wikipedia.org/wiki/Ufa_(nomino)" title="Ufa (nomino) – Swahili" lang="sw" hreflang="sw" data-title="Ufa (nomino)" data-language-autonym="Kiswahili" data-language-local-name="Swahili" class="interlanguage-link-target"><span>Kiswahili</span></a></li><li class="interlanguage-link interwiki-lt mw-list-item"><a href="https://lt.wikipedia.org/wiki/Riftas" title="Riftas – Lithuanian" lang="lt" hreflang="lt" data-title="Riftas" data-language-autonym="Lietuvių" data-language-local-name="Lithuanian" class="interlanguage-link-target"><span>Lietuvių</span></a></li><li class="interlanguage-link interwiki-li mw-list-item"><a href="https://li.wikipedia.org/wiki/Rif_(tektoniek)" title="Rif (tektoniek) – Limburgish" lang="li" hreflang="li" data-title="Rif (tektoniek)" data-language-autonym="Limburgs" data-language-local-name="Limburgish" class="interlanguage-link-target"><span>Limburgs</span></a></li><li class="interlanguage-link interwiki-ms mw-list-item"><a href="https://ms.wikipedia.org/wiki/Rengkahan_benua" title="Rengkahan benua – Malay" lang="ms" hreflang="ms" data-title="Rengkahan benua" data-language-autonym="Bahasa Melayu" data-language-local-name="Malay" 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/Rift" title="Rift – Dutch" lang="nl" hreflang="nl" data-title="Rift" data-language-autonym="Nederlands" data-language-local-name="Dutch" class="interlanguage-link-target"><span>Nederlands</span></a></li><li class="interlanguage-link interwiki-ja mw-list-item"><a href="https://ja.wikipedia.org/wiki/%E3%83%AA%E3%83%95%E3%83%88_(%E5%9C%B0%E8%B3%AA)" title="リフト (地質) – Japanese" lang="ja" hreflang="ja" data-title="リフト (地質)" data-language-autonym="日本語" data-language-local-name="Japanese" class="interlanguage-link-target"><span>日本語</span></a></li><li class="interlanguage-link interwiki-nn mw-list-item"><a href="https://nn.wikipedia.org/wiki/Rift" title="Rift – Norwegian Nynorsk" lang="nn" hreflang="nn" data-title="Rift" data-language-autonym="Norsk nynorsk" data-language-local-name="Norwegian Nynorsk" class="interlanguage-link-target"><span>Norsk nynorsk</span></a></li><li class="interlanguage-link interwiki-oc mw-list-item"><a href="https://oc.wikipedia.org/wiki/Rift" title="Rift – Occitan" lang="oc" hreflang="oc" data-title="Rift" data-language-autonym="Occitan" data-language-local-name="Occitan" class="interlanguage-link-target"><span>Occitan</span></a></li><li class="interlanguage-link interwiki-uz mw-list-item"><a href="https://uz.wikipedia.org/wiki/Rift" title="Rift – Uzbek" lang="uz" hreflang="uz" data-title="Rift" data-language-autonym="Oʻzbekcha / ўзбекча" data-language-local-name="Uzbek" class="interlanguage-link-target"><span>Oʻzbekcha / ўзбекча</span></a></li><li class="interlanguage-link interwiki-pl mw-list-item"><a href="https://pl.wikipedia.org/wiki/Ryft" title="Ryft – Polish" lang="pl" hreflang="pl" data-title="Ryft" data-language-autonym="Polski" data-language-local-name="Polish" 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/Rifte" title="Rifte – Portuguese" lang="pt" hreflang="pt" data-title="Rifte" data-language-autonym="Português" data-language-local-name="Portuguese" class="interlanguage-link-target"><span>Português</span></a></li><li class="interlanguage-link interwiki-ro mw-list-item"><a href="https://ro.wikipedia.org/wiki/Rift" title="Rift – Romanian" lang="ro" hreflang="ro" data-title="Rift" data-language-autonym="Română" data-language-local-name="Romanian" class="interlanguage-link-target"><span>Română</span></a></li><li class="interlanguage-link interwiki-ru mw-list-item"><a href="https://ru.wikipedia.org/wiki/%D0%A0%D0%B8%D1%84%D1%82" title="Рифт – Russian" lang="ru" hreflang="ru" data-title="Рифт" data-language-autonym="Русский" data-language-local-name="Russian" class="interlanguage-link-target"><span>Русский</span></a></li><li class="interlanguage-link interwiki-sah mw-list-item"><a href="https://sah.wikipedia.org/wiki/%D0%A0%D0%B8%D1%84%D1%82" title="Рифт – Yakut" lang="sah" hreflang="sah" data-title="Рифт" data-language-autonym="Саха тыла" data-language-local-name="Yakut" class="interlanguage-link-target"><span>Саха тыла</span></a></li><li class="interlanguage-link interwiki-simple mw-list-item"><a href="https://simple.wikipedia.org/wiki/Rift_(geology)" title="Rift (geology) – Simple English" lang="en-simple" hreflang="en-simple" data-title="Rift (geology)" 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/Rift" title="Rift – Slovak" lang="sk" hreflang="sk" data-title="Rift" data-language-autonym="Slovenčina" data-language-local-name="Slovak" class="interlanguage-link-target"><span>Slovenčina</span></a></li><li class="interlanguage-link interwiki-sr mw-list-item"><a href="https://sr.wikipedia.org/wiki/%D0%A0%D0%B8%D1%84%D1%82" title="Рифт – Serbian" lang="sr" hreflang="sr" data-title="Рифт" data-language-autonym="Српски / srpski" data-language-local-name="Serbian" 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/Rift" title="Rift – Serbo-Croatian" lang="sh" hreflang="sh" data-title="Rift" data-language-autonym="Srpskohrvatski / српскохрватски" data-language-local-name="Serbo-Croatian" class="interlanguage-link-target"><span>Srpskohrvatski / српскохрватски</span></a></li><li class="interlanguage-link interwiki-fi mw-list-item"><a href="https://fi.wikipedia.org/wiki/Hautavajoama" title="Hautavajoama – Finnish" lang="fi" hreflang="fi" data-title="Hautavajoama" data-language-autonym="Suomi" data-language-local-name="Finnish" class="interlanguage-link-target"><span>Suomi</span></a></li><li class="interlanguage-link interwiki-tr mw-list-item"><a href="https://tr.wikipedia.org/wiki/Rift" title="Rift – Turkish" lang="tr" hreflang="tr" data-title="Rift" data-language-autonym="Türkçe" data-language-local-name="Turkish" 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%A0%D0%B8%D1%84%D1%82" title="Рифт – Ukrainian" lang="uk" hreflang="uk" data-title="Рифт" data-language-autonym="Українська" data-language-local-name="Ukrainian" class="interlanguage-link-target"><span>Українська</span></a></li><li class="interlanguage-link interwiki-zh mw-list-item"><a href="https://zh.wikipedia.org/wiki/%E5%BC%B5%E8%A3%82" title="張裂 – Chinese" lang="zh" hreflang="zh" data-title="張裂" 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class="mw-content-ltr mw-parser-output" lang="en" dir="ltr"><div class="shortdescription nomobile noexcerpt noprint searchaux" style="display:none">Geological linear zone where the lithosphere is being pulled apart</div> <style data-mw-deduplicate="TemplateStyles:r1236090951">.mw-parser-output .hatnote{font-style:italic}.mw-parser-output div.hatnote{padding-left:1.6em;margin-bottom:0.5em}.mw-parser-output .hatnote i{font-style:normal}.mw-parser-output .hatnote+link+.hatnote{margin-top:-0.5em}@media print{body.ns-0 .mw-parser-output .hatnote{display:none!important}}</style><div role="note" class="hatnote navigation-not-searchable">"Chasm" redirects here. For other uses, see <a href="/wiki/Chasm_(disambiguation)" class="mw-disambig" title="Chasm (disambiguation)">Chasm (disambiguation)</a>.</div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951" /><div role="note" class="hatnote navigation-not-searchable">This article is about the geological concept. For other uses, see <a href="/wiki/Rift_(disambiguation)" class="mw-disambig" title="Rift (disambiguation)">Rift (disambiguation)</a>.</div> <link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1236090951" /><div role="note" class="hatnote navigation-not-searchable">Not to be confused with <a href="/wiki/Rift_zone" title="Rift zone">rift zone</a>.</div> <figure typeof="mw:File/Thumb"><a href="/wiki/File:Rift_segmentation.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/1/14/Rift_segmentation.png/240px-Rift_segmentation.png" decoding="async" width="240" height="275" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/1/14/Rift_segmentation.png/360px-Rift_segmentation.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/1/14/Rift_segmentation.png/480px-Rift_segmentation.png 2x" data-file-width="650" data-file-height="744" /></a><figcaption>Block view of a rift formed of three segments, showing the location of the accommodation zones between them at changes in fault location or polarity (dip direction)</figcaption></figure> <figure typeof="mw:File/Thumb"><a href="/wiki/File:GulfofSuezRift.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/0/0f/GulfofSuezRift.png/200px-GulfofSuezRift.png" decoding="async" width="200" height="260" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/0/0f/GulfofSuezRift.png/300px-GulfofSuezRift.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/0/0f/GulfofSuezRift.png/400px-GulfofSuezRift.png 2x" data-file-width="2217" data-file-height="2885" /></a><figcaption><a href="/wiki/Gulf_of_Suez_Rift" title="Gulf of Suez Rift">Gulf of Suez Rift</a> showing main <a href="/wiki/Extensional_fault" title="Extensional fault">extensional faults</a></figcaption></figure> <p>In <a href="/wiki/Geology" title="Geology">geology</a>, a <b>rift</b> is a linear zone where the <a href="/wiki/Lithosphere" title="Lithosphere">lithosphere</a> is being pulled apart<sup id="cite_ref-1" class="reference"><a href="#cite_note-1"><span class="cite-bracket">&#91;</span>1<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-2" class="reference"><a href="#cite_note-2"><span class="cite-bracket">&#91;</span>2<span class="cite-bracket">&#93;</span></a></sup> and is an example of <a href="/wiki/Extensional_tectonics" title="Extensional tectonics">extensional tectonics</a>.<sup id="cite_ref-3" class="reference"><a href="#cite_note-3"><span class="cite-bracket">&#91;</span>3<span class="cite-bracket">&#93;</span></a></sup> Typical rift features are a central linear <a href="/wiki/Fault_(geology)" title="Fault (geology)">downfaulted</a> depression, called a <a href="/wiki/Graben" title="Graben">graben</a>, or more commonly a <a href="/wiki/Half-graben" title="Half-graben">half-graben</a> with normal faulting and rift-flank uplifts mainly on one side.<sup id="cite_ref-Leeder_&amp;_Gawthorpe_1987_4-0" class="reference"><a href="#cite_note-Leeder_&amp;_Gawthorpe_1987-4"><span class="cite-bracket">&#91;</span>4<span class="cite-bracket">&#93;</span></a></sup> Where rifts remain above sea level they form a <a href="/wiki/Rift_valley" title="Rift valley">rift valley</a>, which may be filled by water forming a <a href="/wiki/Rift_lake" title="Rift lake">rift lake</a>. The axis of the rift area may contain <a href="/wiki/Volcanic_rocks" class="mw-redirect" title="Volcanic rocks">volcanic rocks</a>, and active <a href="/wiki/Volcanism" title="Volcanism">volcanism</a> is a part of many, but not all, active rift systems. </p><p>Major rifts occur along the central axis of most <a href="/wiki/Mid-ocean_ridge" title="Mid-ocean ridge">mid-ocean ridges</a>, where new <a href="/wiki/Oceanic_crust" title="Oceanic crust">oceanic crust</a> and lithosphere is created along a <a href="/wiki/Divergent_boundary" title="Divergent boundary">divergent boundary</a> between two <a href="/wiki/Tectonic_plate" class="mw-redirect" title="Tectonic plate">tectonic plates</a>. </p><p><i>Failed rifts</i> are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a <a href="/wiki/Triple_junction" title="Triple junction">triple junction</a> where three converging rifts meet over a <a href="/wiki/Hotspot_(geology)" title="Hotspot (geology)">hotspot</a>. Two of these evolve to the point of seafloor spreading, while the third ultimately fails, becoming an <a href="/wiki/Aulacogen" title="Aulacogen">aulacogen</a>. </p> <meta property="mw:PageProp/toc" /> <div class="mw-heading mw-heading2"><h2 id="Geometry">Geometry</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=1" title="Edit section: Geometry"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size mw-halign-left" typeof="mw:File/Thumb"><a href="/wiki/File:FlankMalawi.png" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/d/d8/FlankMalawi.png/250px-FlankMalawi.png" decoding="async" width="220" height="159" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/d/d8/FlankMalawi.png/330px-FlankMalawi.png 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/d/d8/FlankMalawi.png/500px-FlankMalawi.png 2x" data-file-width="5135" data-file-height="3719" /></a><figcaption>Topographic profile of the <a href="/wiki/Malawi_Lake" class="mw-redirect" title="Malawi Lake">Malawi Lake</a></figcaption></figure> <p>Most rifts consist of a series of separate segments that together form the linear zone characteristic of rifts. The individual rift segments have a dominantly half-graben geometry, controlled by a single basin-bounding fault. Segment lengths vary between rifts, depending on the elastic thickness of the lithosphere. </p><p>Areas of thick colder lithosphere, such as the Baikal Rift, have segment lengths in excess of 80&#160;km, while in areas of warmer thin lithosphere, segment lengths may be less than 30&#160;km.<sup id="cite_ref-Ebinger_5-0" class="reference"><a href="#cite_note-Ebinger-5"><span class="cite-bracket">&#91;</span>5<span class="cite-bracket">&#93;</span></a></sup> Along the axis of the rift the position, and in some cases the polarity (the dip direction), of the main rift bounding fault changes from segment to segment. Segment boundaries often have a more complex structure and generally cross the rift axis at a high angle. These segment boundary zones accommodate the differences in fault displacement between the segments and are therefore known as accommodation zones. </p><p>Accommodation zones take various forms, from a simple relay ramp at the overlap between two major faults of the same polarity, to zones of high structural complexity, particularly where the segments have opposite polarity. Accommodation zones may be located where older crustal structures intersect the rift axis. In the Gulf of Suez rift, the Zaafarana accommodation zone is located where a <a href="/wiki/Shear_zone" title="Shear zone">shear zone</a> in the <a href="/wiki/Arabian-Nubian_Shield" title="Arabian-Nubian Shield">Arabian-Nubian Shield</a> meets the rift.<sup id="cite_ref-Younes_6-0" class="reference"><a href="#cite_note-Younes-6"><span class="cite-bracket">&#91;</span>6<span class="cite-bracket">&#93;</span></a></sup> </p><p>Rift flanks or shoulders are elevated areas around rifts. Rift shoulders are typically about 70&#160;km wide.<sup id="cite_ref-Greenetal2018_7-0" class="reference"><a href="#cite_note-Greenetal2018-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup> Contrary to what was previously thought, elevated passive continental margins (EPCM) such as the <a href="/wiki/Brazilian_Highlands" title="Brazilian Highlands">Brazilian Highlands</a>, the <a href="/wiki/Scandinavian_Mountains#Origin" title="Scandinavian Mountains">Scandinavian Mountains</a> and India's <a href="/wiki/Western_Ghats" title="Western Ghats">Western Ghats</a>, are not rift shoulders.<sup id="cite_ref-Greenetal2018_7-1" class="reference"><a href="#cite_note-Greenetal2018-7"><span class="cite-bracket">&#91;</span>7<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Rift_development">Rift development</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=2" title="Edit section: Rift development"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <div class="mw-heading mw-heading3"><h3 id="Rift_initiation">Rift initiation</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=3" title="Edit section: Rift initiation"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The formation of rift basins and strain localization reflects rift maturity. At the onset of rifting, the upper part of the lithosphere starts to extend on a series of initially unconnected <a href="/wiki/Normal_fault" class="mw-redirect" title="Normal fault">normal faults</a>, leading to the development of isolated basins.<sup id="cite_ref-Withjack_8-0" class="reference"><a href="#cite_note-Withjack-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> In subaerial rifts, for example, drainage at the onset of rifting is generally internal, with no element of through drainage. </p> <div class="mw-heading mw-heading3"><h3 id="Mature_rift_stage">Mature rift stage</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=4" title="Edit section: Mature rift stage"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>As the rift evolves, some of the individual fault segments grow, eventually becoming linked together to form the larger bounding faults. Subsequent extension becomes concentrated on these faults. The longer faults and wider fault spacing leads to more continuous areas of fault-related <a href="/wiki/Subsidence" title="Subsidence">subsidence</a> along the rift axis. Significant uplift of the rift shoulders develops at this stage, strongly influencing drainage and sedimentation in the rift basins.<sup id="cite_ref-Withjack_8-1" class="reference"><a href="#cite_note-Withjack-8"><span class="cite-bracket">&#91;</span>8<span class="cite-bracket">&#93;</span></a></sup> </p><p>During the climax of lithospheric rifting, as the crust is thinned, the Earth's surface subsides and the <a href="/wiki/Mohorovi%C4%8Di%C4%87_discontinuity" title="Mohorovičić discontinuity">Moho</a> becomes correspondingly raised. At the same time, the mantle lithosphere becomes thinned, causing a rise of the top of the asthenosphere. This brings high heat flow from the upwelling asthenosphere into the thinning lithosphere, heating the orogenic lithosphere for dehydration melting, typically causing extreme metamorphism at high thermal gradients of greater than 30&#160;°C. The metamorphic products are high to ultrahigh temperature granulites and their associated migmatite and granites in collisional orogens, with possible emplacement of metamorphic core complexes in continental rift zones but oceanic core complexes in spreading ridges. This leads to a kind of orogeneses in extensional settings, which is referred as to rifting orogeny.<sup id="cite_ref-9" class="reference"><a href="#cite_note-9"><span class="cite-bracket">&#91;</span>9<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Post-rift_subsidence">Post-rift subsidence</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=5" title="Edit section: Post-rift subsidence"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Once rifting ceases, the mantle beneath the rift cools and this is accompanied by a broad area of post-rift subsidence. The amount of subsidence is directly related to the amount of thinning during the rifting phase calculated as the beta factor (initial crustal thickness divided by final crustal thickness), but is also affected by the degree to which the rift basin is filled at each stage, due to the greater density of sediments in contrast to water. The simple 'McKenzie model' of rifting, which considers the rifting stage to be instantaneous, provides a good first order estimate of the amount of crustal thinning from observations of the amount of post-rift subsidence.<sup id="cite_ref-McKenzie_10-0" class="reference"><a href="#cite_note-McKenzie-10"><span class="cite-bracket">&#91;</span>10<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Kusznir_11-0" class="reference"><a href="#cite_note-Kusznir-11"><span class="cite-bracket">&#91;</span>11<span class="cite-bracket">&#93;</span></a></sup> This has generally been replaced by the 'flexural cantilever model', which takes into account the geometry of the rift faults and the <a href="/wiki/Lithospheric_flexure" title="Lithospheric flexure">flexural</a> <a href="/wiki/Isostasy" title="Isostasy">isostasy</a> of the upper part of the crust.<sup id="cite_ref-Nøttvedt_12-0" class="reference"><a href="#cite_note-Nøttvedt-12"><span class="cite-bracket">&#91;</span>12<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Multiphase_rifting">Multiphase rifting</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=6" title="Edit section: Multiphase rifting"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Some rifts show a complex and prolonged history of rifting, with several distinct phases. The <a href="/wiki/Geology_of_the_North_Sea" title="Geology of the North Sea">North Sea rift</a> shows evidence of several separate rift phases from the <a href="/wiki/Permian" title="Permian">Permian</a> through to the Earliest <a href="/wiki/Cretaceous" title="Cretaceous">Cretaceous</a>,<sup id="cite_ref-Rodmar_13-0" class="reference"><a href="#cite_note-Rodmar-13"><span class="cite-bracket">&#91;</span>13<span class="cite-bracket">&#93;</span></a></sup> a period of over 100 million years. </p> <div class="mw-heading mw-heading3"><h3 id="Rifting_to_break-up">Rifting to break-up</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=7" title="Edit section: Rifting to break-up"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Rifting may lead to continental breakup and formation of oceanic basins. Successful rifting leads to seafloor spreading along a mid-oceanic ridge and a set of conjugate margins separated by an oceanic basin.<sup id="cite_ref-14" class="reference"><a href="#cite_note-14"><span class="cite-bracket">&#91;</span>14<span class="cite-bracket">&#93;</span></a></sup> Rifting may be active, and controlled by <a href="/wiki/Mantle_convection" title="Mantle convection">mantle convection</a>. It may also be passive, and driven by far-field tectonic forces that stretch the lithosphere. Margin architecture develops due to spatial and temporal relationships between extensional deformation phases. Margin segmentation eventually leads to the formation of rift domains with variations of the <a href="/wiki/Mohorovi%C4%8Di%C4%87_discontinuity" title="Mohorovičić discontinuity">Moho</a> topography, including proximal domain with fault-rotated crustal blocks, necking zone with thinning of crustal <a href="/wiki/Basement_(geology)" title="Basement (geology)">basement</a>, distal domain with deep sag basins, ocean-continent transition and oceanic domain.<sup id="cite_ref-Marine_and_Petroleum_Geology_15-0" class="reference"><a href="#cite_note-Marine_and_Petroleum_Geology-15"><span class="cite-bracket">&#91;</span>15<span class="cite-bracket">&#93;</span></a></sup> </p><p>Deformation and magmatism interact during rift evolution. Magma-rich and magma-poor rifted margins may be formed.<sup id="cite_ref-Marine_and_Petroleum_Geology_15-1" class="reference"><a href="#cite_note-Marine_and_Petroleum_Geology-15"><span class="cite-bracket">&#91;</span>15<span class="cite-bracket">&#93;</span></a></sup> Magma-rich margins include major volcanic features. Globally, volcanic margins represent the majority of passive continental margins.<sup id="cite_ref-16" class="reference"><a href="#cite_note-16"><span class="cite-bracket">&#91;</span>16<span class="cite-bracket">&#93;</span></a></sup> Magma-starved rifted margins are affected by large-scale faulting and crustal hyperextension.<sup id="cite_ref-17" class="reference"><a href="#cite_note-17"><span class="cite-bracket">&#91;</span>17<span class="cite-bracket">&#93;</span></a></sup> As a consequence, upper mantle peridotites and gabbros are commonly exposed and serpentinized along extensional detachments at the seafloor. </p> <div class="mw-heading mw-heading2"><h2 id="Magmatism">Magmatism</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=8" title="Edit section: Magmatism"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <figure class="mw-default-size" typeof="mw:File/Thumb"><a href="/wiki/File:20190621_CPH-KEF_7314_(48453477346).jpg" class="mw-file-description"><img src="//upload.wikimedia.org/wikipedia/commons/thumb/7/7a/20190621_CPH-KEF_7314_%2848453477346%29.jpg/330px-20190621_CPH-KEF_7314_%2848453477346%29.jpg" decoding="async" width="300" height="200" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/7/7a/20190621_CPH-KEF_7314_%2848453477346%29.jpg/500px-20190621_CPH-KEF_7314_%2848453477346%29.jpg 1.5x, //upload.wikimedia.org/wikipedia/commons/thumb/7/7a/20190621_CPH-KEF_7314_%2848453477346%29.jpg/960px-20190621_CPH-KEF_7314_%2848453477346%29.jpg 2x" data-file-width="7952" data-file-height="5304" /></a><figcaption>Volcano-tectonic landforms connected to rifting on <a href="/wiki/Geology_of_Reykjanes_Peninsula" title="Geology of Reykjanes Peninsula">Reykjanes Peninsula</a>, <a href="/wiki/Iceland" title="Iceland">Iceland</a>: <a href="/wiki/Fault_(geology)" title="Fault (geology)">faults</a>, <a href="/wiki/Fissure_vent" title="Fissure vent">fissures</a>, elongated <a href="/wiki/Volcano" title="Volcano">volcanoes</a> of <a href="/wiki/Subglacial_volcano" title="Subglacial volcano">subglacial origin</a>, postglacial <a href="/wiki/Lava_field" title="Lava field">lava fields</a></figcaption></figure> <p>Many rifts are the sites of at least minor <a href="/wiki/Magmatism" title="Magmatism">magmatic activity</a>, particularly in the early stages of rifting.<sup id="cite_ref-White_18-0" class="reference"><a href="#cite_note-White-18"><span class="cite-bracket">&#91;</span>18<span class="cite-bracket">&#93;</span></a></sup> <a href="/wiki/Alkali_basalt" title="Alkali basalt">Alkali basalts</a> and <a href="/wiki/Bimodal_volcanism" title="Bimodal volcanism">bimodal volcanism</a> are common products of rift-related magmatism.<sup id="cite_ref-Farmer_19-0" class="reference"><a href="#cite_note-Farmer-19"><span class="cite-bracket">&#91;</span>19<span class="cite-bracket">&#93;</span></a></sup><sup id="cite_ref-Cas_20-0" class="reference"><a href="#cite_note-Cas-20"><span class="cite-bracket">&#91;</span>20<span class="cite-bracket">&#93;</span></a></sup> </p><p>Recent studies indicate that post-collisional granites in collisional orogens are the product of rifting magmatism at converged plate margins.<sup class="noprint Inline-Template Template-Fact" style="white-space:nowrap;">&#91;<i><a href="/wiki/Wikipedia:Citation_needed" title="Wikipedia:Citation needed"><span title="This claim needs references to reliable sources. (October 2018)">citation needed</span></a></i>&#93;</sup> </p> <div class="mw-heading mw-heading2"><h2 id="Economic_importance">Economic importance</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=9" title="Edit section: Economic importance"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>The sedimentary rocks associated with continental rifts host important deposits of both minerals and <a href="/wiki/Hydrocarbon" title="Hydrocarbon">hydrocarbons</a>.<sup id="cite_ref-USGS_21-0" class="reference"><a href="#cite_note-USGS-21"><span class="cite-bracket">&#91;</span>21<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Mineral_deposits">Mineral deposits</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=10" title="Edit section: Mineral deposits"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p><a href="/wiki/Sedimentary_exhalative_deposits" title="Sedimentary exhalative deposits">SedEx</a> mineral deposits are found mainly in continental rift settings. They form within post-rift sequences when hydrothermal fluids associated with magmatic activity are expelled at the seabed.<sup id="cite_ref-Groves_22-0" class="reference"><a href="#cite_note-Groves-22"><span class="cite-bracket">&#91;</span>22<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading3"><h3 id="Oil_and_gas">Oil and gas</h3><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=11" title="Edit section: Oil and gas"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <p>Continental rifts are the sites of significant oil and gas accumulations, such as the <a href="/wiki/Geology_of_the_North_Sea" title="Geology of the North Sea">Viking Graben</a> and the <a href="/wiki/Gulf_of_Suez_Rift" title="Gulf of Suez Rift">Gulf of Suez Rift</a>. Thirty percent of <a href="/wiki/Giant_oil_and_gas_fields" title="Giant oil and gas fields">giant oil and gas fields</a> are found within such a setting.<sup id="cite_ref-Mann_23-0" class="reference"><a href="#cite_note-Mann-23"><span class="cite-bracket">&#91;</span>23<span class="cite-bracket">&#93;</span></a></sup> In 1999 it was estimated that there were 200 <a href="/wiki/1000000000_(number)" class="mw-redirect" title="1000000000 (number)">billion</a> <a href="/wiki/Barrel_(unit)#Oil_barrel" title="Barrel (unit)">barrels</a> of recoverable oil reserves hosted in rifts. <a href="/wiki/Source_rock" title="Source rock">Source rocks</a> are often developed within the sediments filling the active rift (<a href="/wiki/Tectonostratigraphy#Effects_of_active_tectonics_on_lithostratigraphy" title="Tectonostratigraphy">syn-rift</a>), forming either in a <a href="https://en.wiktionary.org/wiki/lacustrine" class="extiw" title="wikt:lacustrine">lacustrine</a> environment or in a restricted marine environment, although not all rifts contain such sequences. <a href="/wiki/Petroleum_reservoir" title="Petroleum reservoir">Reservoir rocks</a> may be developed in pre-rift, syn-rift and post-rift sequences. </p><p>Effective regional seals may be present within the post-rift sequence if <a href="/wiki/Mudstone" title="Mudstone">mudstones</a> or <a href="/wiki/Evaporite" title="Evaporite">evaporites</a> are deposited. Just over half of estimated oil reserves are found associated with rifts containing marine syn-rift and post-rift sequences, just under a quarter in rifts with a non-marine syn-rift and post-rift, and an eighth in non-marine syn-rift with a marine post-rift.<sup id="cite_ref-Lambiase_24-0" class="reference"><a href="#cite_note-Lambiase-24"><span class="cite-bracket">&#91;</span>24<span class="cite-bracket">&#93;</span></a></sup> </p> <div class="mw-heading mw-heading2"><h2 id="Examples">Examples</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=12" title="Edit section: Examples"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <ul><li>The <a href="/wiki/Asunci%C3%B3n_Rift" title="Asunción Rift">Asunción Rift</a> in Eastern Paraguay</li> <li>The <a href="/wiki/Canadian_Arctic_Rift_System" title="Canadian Arctic Rift System">Canadian Arctic Rift System</a> in northern <a href="/wiki/North_America" title="North America">North America</a></li> <li>The <a href="/wiki/East_African_Rift" title="East African Rift">East African Rift</a></li> <li>The <a href="/wiki/West_and_Central_African_Rift_System" title="West and Central African Rift System">West and Central African Rift System</a></li> <li>The <a href="/wiki/Red_Sea_Rift" title="Red Sea Rift">Red Sea Rift</a></li> <li>The <a href="/wiki/Gulf_of_California" title="Gulf of California">Gulf of California</a></li> <li>The <a href="/wiki/Baikal_Rift_Zone" title="Baikal Rift Zone">Baikal Rift Zone</a>, the bottom of <a href="/wiki/Lake_Baikal" title="Lake Baikal">Lake Baikal</a> is the deepest continental rift on the earth.</li> <li>The <a href="/wiki/Gulf_of_Suez_Rift" title="Gulf of Suez Rift">Gulf of Suez Rift</a></li> <li>Throughout the <a href="/wiki/Basin_and_Range_Province" title="Basin and Range Province">Basin and Range Province</a> in North America</li> <li>The <a href="/wiki/Rio_Grande_Rift" class="mw-redirect" title="Rio Grande Rift">Rio Grande Rift</a> in the southwestern US</li> <li>The rift zone that contains the <a href="/wiki/Gulf_of_Corinth" title="Gulf of Corinth">Gulf of Corinth</a> in <a href="/wiki/Greece" title="Greece">Greece</a></li> <li>The <a href="/wiki/Reelfoot_Rift" class="mw-redirect" title="Reelfoot Rift">Reelfoot Rift</a>, an ancient buried failed rift underlying the <a href="/wiki/New_Madrid_Seismic_Zone" class="mw-redirect" title="New Madrid Seismic Zone">New Madrid Seismic Zone</a> in the <a href="/wiki/Mississippi_embayment" title="Mississippi embayment">Mississippi embayment</a></li> <li>The <a href="/wiki/Rhine_Rift" class="mw-redirect" title="Rhine Rift">Rhine Rift</a>, in southwestern Germany, known as the <a href="/wiki/Upper_Rhine_valley" class="mw-redirect" title="Upper Rhine valley">Upper Rhine valley</a>, part of the <a href="/wiki/European_Cenozoic_Rift_System" title="European Cenozoic Rift System">European Cenozoic Rift System</a></li> <li>The <a href="/wiki/Taup%C5%8D_Volcanic_Zone" title="Taupō Volcanic Zone">Taupō Volcanic Zone</a> in the <a href="/wiki/North_Island" title="North Island">North Island</a> of <a href="/wiki/New_Zealand" title="New Zealand">New Zealand</a></li> <li>The <a href="/wiki/Oslo_Graben" title="Oslo Graben">Oslo Graben</a> in <a href="/wiki/Norway" title="Norway">Norway</a></li> <li>The <a href="/wiki/Ottawa-Bonnechere_Graben" title="Ottawa-Bonnechere Graben">Ottawa-Bonnechere Graben</a> in Ontario and Quebec</li> <li>The <a href="/wiki/Northern_Cordilleran_Volcanic_Province" title="Northern Cordilleran Volcanic Province">Northern Cordilleran Volcanic Province</a> in <a href="/wiki/British_Columbia" title="British Columbia">British Columbia</a>, <a href="/wiki/Yukon" title="Yukon">Yukon</a> and <a href="/wiki/Alaska" title="Alaska">Alaska</a></li> <li>The <a href="/wiki/West_Antarctic_Rift_System" title="West Antarctic Rift System">West Antarctic Rift System</a> in <a href="/wiki/Antarctica" title="Antarctica">Antarctica</a></li> <li>The <a href="/wiki/Midcontinent_Rift_System" title="Midcontinent Rift System">Midcontinent Rift System</a>, a late <a href="/wiki/Precambrian" title="Precambrian">Precambrian</a> rift in central North America</li> <li>The <a href="/wiki/Central_Lowlands" title="Central Lowlands">Midland Valley</a> in Scotland</li> <li>The <a href="/wiki/Fundy_Basin" title="Fundy Basin">Fundy Basin</a>, a <a href="/wiki/Triassic" title="Triassic">Triassic</a> rift basin in southeastern Canada</li> <li>The Cambay, Kachchh, and Narmada rifts<sup id="cite_ref-25" class="reference"><a href="#cite_note-25"><span class="cite-bracket">&#91;</span>25<span class="cite-bracket">&#93;</span></a></sup> in northwestern <a href="/wiki/Deccan_Traps" title="Deccan Traps">Deccan volcanic province</a> of India<sup id="cite_ref-26" class="reference"><a href="#cite_note-26"><span class="cite-bracket">&#91;</span>26<span class="cite-bracket">&#93;</span></a></sup></li></ul> <div class="mw-heading mw-heading2"><h2 id="See_also">See also</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=13" title="Edit section: See also"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1266661725">.mw-parser-output .portalbox{padding:0;margin:0.5em 0;display:table;box-sizing:border-box;max-width:175px;list-style:none}.mw-parser-output .portalborder{border:1px solid var(--border-color-base,#a2a9b1);padding:0.1em;background:var(--background-color-neutral-subtle,#f8f9fa)}.mw-parser-output .portalbox-entry{display:table-row;font-size:85%;line-height:110%;height:1.9em;font-style:italic;font-weight:bold}.mw-parser-output .portalbox-image{display:table-cell;padding:0.2em;vertical-align:middle;text-align:center}.mw-parser-output .portalbox-link{display:table-cell;padding:0.2em 0.2em 0.2em 0.3em;vertical-align:middle}@media(min-width:720px){.mw-parser-output .portalleft{margin:0.5em 1em 0.5em 0}.mw-parser-output .portalright{clear:right;float:right;margin:0.5em 0 0.5em 1em}}</style><ul role="navigation" aria-label="Portals" class="noprint portalbox portalborder portalright"> <li class="portalbox-entry"><span class="portalbox-image"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:WikiProject_Geology.svg" class="mw-file-description"><img alt="icon" src="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/WikiProject_Geology.svg/40px-WikiProject_Geology.svg.png" decoding="async" width="28" height="28" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/commons/thumb/e/e7/WikiProject_Geology.svg/60px-WikiProject_Geology.svg.png 1.5x" data-file-width="327" data-file-height="328" /></a></span></span><span class="portalbox-link"><a href="/wiki/Portal:Geology" title="Portal:Geology">Geology portal</a></span></li></ul> <ul><li><a href="/wiki/Rift_zone" title="Rift zone">Rift zone</a></li> <li><a href="/wiki/Wilson_Cycle" title="Wilson Cycle">Wilson Cycle</a></li></ul> <div class="mw-heading mw-heading2"><h2 id="References">References</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=14" title="Edit section: References"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1239543626">.mw-parser-output .reflist{margin-bottom:0.5em;list-style-type:decimal}@media screen{.mw-parser-output .reflist{font-size:90%}}.mw-parser-output .reflist .references{font-size:100%;margin-bottom:0;list-style-type:inherit}.mw-parser-output .reflist-columns-2{column-width:30em}.mw-parser-output .reflist-columns-3{column-width:25em}.mw-parser-output .reflist-columns{margin-top:0.3em}.mw-parser-output .reflist-columns ol{margin-top:0}.mw-parser-output .reflist-columns li{page-break-inside:avoid;break-inside:avoid-column}.mw-parser-output .reflist-upper-alpha{list-style-type:upper-alpha}.mw-parser-output .reflist-upper-roman{list-style-type:upper-roman}.mw-parser-output .reflist-lower-alpha{list-style-type:lower-alpha}.mw-parser-output .reflist-lower-greek{list-style-type:lower-greek}.mw-parser-output .reflist-lower-roman{list-style-type:lower-roman}</style><div class="reflist reflist-columns references-column-width" style="column-width: 33em;"> <ol class="references"> <li id="cite_note-1"><span class="mw-cite-backlink"><b><a href="#cite_ref-1">^</a></b></span> <span class="reference-text"><a rel="nofollow" class="external text" href="http://ethiopianrift.igg.cnr.it/rift%20valley%20significance.htm">Rift valley: definition and geologic significance</a>, Giacomo Corti, The Ethiopian Rift Valley</span> </li> <li id="cite_note-2"><span class="mw-cite-backlink"><b><a href="#cite_ref-2">^</a></b></span> <span class="reference-text"><a rel="nofollow" class="external text" href="http://www.mantleplumes.org/VM_DecompressMelt.html">Decompressional Melting During Extension of Continental Lithosphere</a>, Jolante van Wijk, MantlePlumes.org</span> </li> <li id="cite_note-3"><span class="mw-cite-backlink"><b><a href="#cite_ref-3">^</a></b></span> <span class="reference-text"><a rel="nofollow" class="external text" href="http://www.le.ac.uk/geology/art/gl209/lecture4/lecture4.html">Plate Tectonics: Lecture 2</a>, Geology Department at University of Leicester</span> </li> <li id="cite_note-Leeder_&amp;_Gawthorpe_1987-4"><span class="mw-cite-backlink"><b><a href="#cite_ref-Leeder_&amp;_Gawthorpe_1987_4-0">^</a></b></span> <span class="reference-text"><style data-mw-deduplicate="TemplateStyles:r1238218222">.mw-parser-output cite.citation{font-style:inherit;word-wrap:break-word}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .citation:target{background-color:rgba(0,127,255,0.133)}.mw-parser-output .id-lock-free.id-lock-free a{background:url("//upload.wikimedia.org/wikipedia/commons/6/65/Lock-green.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-limited.id-lock-limited a,.mw-parser-output .id-lock-registration.id-lock-registration a{background:url("//upload.wikimedia.org/wikipedia/commons/d/d6/Lock-gray-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .id-lock-subscription.id-lock-subscription a{background:url("//upload.wikimedia.org/wikipedia/commons/a/aa/Lock-red-alt-2.svg")right 0.1em center/9px no-repeat}.mw-parser-output .cs1-ws-icon a{background:url("//upload.wikimedia.org/wikipedia/commons/4/4c/Wikisource-logo.svg")right 0.1em center/12px no-repeat}body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-free a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-limited a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-registration a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .id-lock-subscription a,body:not(.skin-timeless):not(.skin-minerva) .mw-parser-output .cs1-ws-icon a{background-size:contain;padding:0 1em 0 0}.mw-parser-output .cs1-code{color:inherit;background:inherit;border:none;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;color:var(--color-error,#d33)}.mw-parser-output .cs1-visible-error{color:var(--color-error,#d33)}.mw-parser-output .cs1-maint{display:none;color:#085;margin-left:0.3em}.mw-parser-output .cs1-kern-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right{padding-right:0.2em}.mw-parser-output .citation .mw-selflink{font-weight:inherit}@media screen{.mw-parser-output .cs1-format{font-size:95%}html.skin-theme-clientpref-night .mw-parser-output .cs1-maint{color:#18911f}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .cs1-maint{color:#18911f}}</style><cite id="CITEREFLeederGawthorpe1987" class="citation book cs1">Leeder, M.R.; Gawthorpe, R.L. 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"Hydrocarbons in rift basins: the role of stratigraphy". <i><a href="/wiki/Philosophical_Transactions_of_the_Royal_Society_A" title="Philosophical Transactions of the Royal Society A">Philosophical Transactions of the Royal Society A</a></i>. <b>357</b> (1753): <span class="nowrap">877–</span>900. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1999RSPTA.357..877L">1999RSPTA.357..877L</a>. <a href="/wiki/CiteSeerX_(identifier)" class="mw-redirect" title="CiteSeerX (identifier)">CiteSeerX</a>&#160;<span class="id-lock-free" title="Freely accessible"><a rel="nofollow" class="external text" href="https://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.892.6422">10.1.1.892.6422</a></span>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1098%2Frsta.1999.0356">10.1098/rsta.1999.0356</a>. <a href="/wiki/S2CID_(identifier)" class="mw-redirect" title="S2CID (identifier)">S2CID</a>&#160;<a rel="nofollow" class="external text" href="https://api.semanticscholar.org/CorpusID:129564482">129564482</a>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Philosophical+Transactions+of+the+Royal+Society+A&amp;rft.atitle=Hydrocarbons+in+rift+basins%3A+the+role+of+stratigraphy&amp;rft.volume=357&amp;rft.issue=1753&amp;rft.pages=%3Cspan+class%3D%22nowrap%22%3E877-%3C%2Fspan%3E900&amp;rft.date=1999&amp;rft_id=https%3A%2F%2Fciteseerx.ist.psu.edu%2Fviewdoc%2Fsummary%3Fdoi%3D10.1.1.892.6422%23id-name%3DCiteSeerX&amp;rft_id=https%3A%2F%2Fapi.semanticscholar.org%2FCorpusID%3A129564482%23id-name%3DS2CID&amp;rft_id=info%3Adoi%2F10.1098%2Frsta.1999.0356&amp;rft_id=info%3Abibcode%2F1999RSPTA.357..877L&amp;rft.aulast=Lambiase&amp;rft.aufirst=J.J.&amp;rft.au=Morley+C.K.&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ARift" class="Z3988"></span></span> </li> <li id="cite_note-25"><span class="mw-cite-backlink"><b><a href="#cite_ref-25">^</a></b></span> <span class="reference-text">Chouhan, A.K. Structural fabric over the seismically active Kachchh rift basin, India: insight from world gravity model 2012. Environ Earth Sci 79, 316 (2020). <a rel="nofollow" class="external free" href="https://doi.org/10.1007/s12665-020-09068-2">https://doi.org/10.1007/s12665-020-09068-2</a></span> </li> <li id="cite_note-26"><span class="mw-cite-backlink"><b><a href="#cite_ref-26">^</a></b></span> <span class="reference-text">Chouhan, A.K., Choudhury, P. &amp; Pal, S.K. New evidence for a thin crust and magmatic underplating beneath the Cambay rift basin, Western India through modelling of EIGEN-6C4 gravity data. J Earth Syst Sci 129, 64 (2020). <a rel="nofollow" class="external free" href="https://doi.org/10.1007/s12040-019-1335-y">https://doi.org/10.1007/s12040-019-1335-y</a></span> </li> </ol></div> <div class="mw-heading mw-heading2"><h2 id="Further_reading">Further reading</h2><span class="mw-editsection"><span class="mw-editsection-bracket">[</span><a href="/w/index.php?title=Rift&amp;action=edit&amp;section=15" title="Edit section: Further reading"><span>edit</span></a><span class="mw-editsection-bracket">]</span></span></div> <style data-mw-deduplicate="TemplateStyles:r1235681985">.mw-parser-output .side-box{margin:4px 0;box-sizing:border-box;border:1px solid #aaa;font-size:88%;line-height:1.25em;background-color:var(--background-color-interactive-subtle,#f8f9fa);display:flow-root}.mw-parser-output .side-box-abovebelow,.mw-parser-output .side-box-text{padding:0.25em 0.9em}.mw-parser-output .side-box-image{padding:2px 0 2px 0.9em;text-align:center}.mw-parser-output .side-box-imageright{padding:2px 0.9em 2px 0;text-align:center}@media(min-width:500px){.mw-parser-output .side-box-flex{display:flex;align-items:center}.mw-parser-output .side-box-text{flex:1;min-width:0}}@media(min-width:720px){.mw-parser-output .side-box{width:238px}.mw-parser-output .side-box-right{clear:right;float:right;margin-left:1em}.mw-parser-output .side-box-left{margin-right:1em}}</style><style data-mw-deduplicate="TemplateStyles:r1237033735">@media print{body.ns-0 .mw-parser-output .sistersitebox{display:none!important}}@media screen{html.skin-theme-clientpref-night .mw-parser-output .sistersitebox img[src*="Wiktionary-logo-en-v2.svg"]{background-color:white}}@media screen and (prefers-color-scheme:dark){html.skin-theme-clientpref-os .mw-parser-output .sistersitebox img[src*="Wiktionary-logo-en-v2.svg"]{background-color:white}}</style><div class="side-box side-box-right plainlinks sistersitebox"><style data-mw-deduplicate="TemplateStyles:r1126788409">.mw-parser-output .plainlist ol,.mw-parser-output .plainlist ul{line-height:inherit;list-style:none;margin:0;padding:0}.mw-parser-output .plainlist ol li,.mw-parser-output .plainlist ul li{margin-bottom:0}</style> <div class="side-box-flex"> <div class="side-box-image"><span class="noviewer" typeof="mw:File"><a href="/wiki/File:Commons-logo.svg" class="mw-file-description"><img alt="" src="//upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/40px-Commons-logo.svg.png" decoding="async" width="30" height="40" class="mw-file-element" srcset="//upload.wikimedia.org/wikipedia/en/thumb/4/4a/Commons-logo.svg/60px-Commons-logo.svg.png 1.5x" data-file-width="1024" data-file-height="1376" /></a></span></div> <div class="side-box-text plainlist">Wikimedia Commons has media related to <span style="font-weight: bold; font-style: italic;"><a href="https://commons.wikimedia.org/wiki/Category:Rifts" class="extiw" title="commons:Category:Rifts">Rifts</a></span>.</div></div> </div> <ul><li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFBallySnelson1980" class="citation journal cs1">Bally, A.W.; Snelson, S. (1980). "Realms of subsidence". <i>Canadian Society for Petroleum Geology Memoir</i>. <b>6</b>: <span class="nowrap">9–</span>94.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=Canadian+Society+for+Petroleum+Geology+Memoir&amp;rft.atitle=Realms+of+subsidence&amp;rft.volume=6&amp;rft.pages=%3Cspan+class%3D%22nowrap%22%3E9-%3C%2Fspan%3E94&amp;rft.date=1980&amp;rft.aulast=Bally&amp;rft.aufirst=A.W.&amp;rft.au=Snelson%2C+S.&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ARift" class="Z3988"></span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFKingstonDishroonWilliams1983" class="citation journal cs1">Kingston, D.R.; Dishroon, C.P.; Williams, P.A. (December 1983). <a rel="nofollow" class="external text" href="http://www.monografias.com/trabajos-pdf4/global-basin-classification-system/global-basin-classification-system.pdf">"Global Basin Classification System"</a> <span class="cs1-format">(PDF)</span>. <i><a href="/wiki/American_Association_of_Petroleum_Geologists" title="American Association of Petroleum Geologists">AAPG Bulletin</a></i>. <b>67</b> (12): <span class="nowrap">2175–</span>2193<span class="reference-accessdate">. Retrieved <span class="nowrap">2017-06-23</span></span>.</cite><span title="ctx_ver=Z39.88-2004&amp;rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&amp;rft.genre=article&amp;rft.jtitle=AAPG+Bulletin&amp;rft.atitle=Global+Basin+Classification+System&amp;rft.volume=67&amp;rft.issue=12&amp;rft.pages=%3Cspan+class%3D%22nowrap%22%3E2175-%3C%2Fspan%3E2193&amp;rft.date=1983-12&amp;rft.aulast=Kingston&amp;rft.aufirst=D.R.&amp;rft.au=Dishroon%2C+C.P.&amp;rft.au=Williams%2C+P.A.&amp;rft_id=http%3A%2F%2Fwww.monografias.com%2Ftrabajos-pdf4%2Fglobal-basin-classification-system%2Fglobal-basin-classification-system.pdf&amp;rfr_id=info%3Asid%2Fen.wikipedia.org%3ARift" class="Z3988"></span></li> <li><link rel="mw-deduplicated-inline-style" href="mw-data:TemplateStyles:r1238218222" /><cite id="CITEREFKlemme1980" class="citation journal cs1">Klemme, H.D (1980). "Petroleum Basins - Classifications and Characteristics". <i><a href="/wiki/Journal_of_Petroleum_Geology" title="Journal of Petroleum Geology">Journal of Petroleum Geology</a></i>. <b>3</b> (2): <span class="nowrap">187–</span>207. <a href="/wiki/Bibcode_(identifier)" class="mw-redirect" title="Bibcode (identifier)">Bibcode</a>:<a rel="nofollow" class="external text" href="https://ui.adsabs.harvard.edu/abs/1980JPetG...3..187K">1980JPetG...3..187K</a>. <a href="/wiki/Doi_(identifier)" class="mw-redirect" title="Doi (identifier)">doi</a>:<a rel="nofollow" class="external text" href="https://doi.org/10.1111%2Fj.1747-5457.1980.tb00982.x">10.1111/j.1747-5457.1980.tb00982.x</a>.</cite><span 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href="/wiki/Mohr%E2%80%93Coulomb_theory" title="Mohr–Coulomb theory">Mohr–Coulomb theory</a></li> <li><a href="/wiki/Mohr%27s_circle" title="Mohr&#39;s circle">Mohr's circle</a></li> <li><a href="/wiki/Overburden_pressure" title="Overburden pressure">Overburden pressure</a></li> <li><a href="/wiki/Rock_mechanics" title="Rock mechanics">Rock mechanics</a></li> <li><a href="/wiki/Deformation_(physics)" title="Deformation (physics)">Strain</a></li> <li><a href="/wiki/Strain_partitioning" title="Strain partitioning">Strain partitioning</a></li> <li><a href="/wiki/Stress_(mechanics)" title="Stress (mechanics)">Stress</a></li> <li><a href="/wiki/Stress_field" title="Stress field">Stress field</a></li> <li><a href="/wiki/Tension_(geology)" title="Tension (geology)">Tension</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Measurement conventions</th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Brunton_compass" title="Brunton compass">Brunton compass</a></li> <li><a href="/wiki/Inclinometer" title="Inclinometer">Inclinometer</a></li> <li><a href="/wiki/Orthographic_projection" title="Orthographic projection">Orthographic projection</a></li> <li><a href="/wiki/Rake_(geology)" title="Rake (geology)">Rake</a></li> <li><a href="/wiki/Stereographic_projection" title="Stereographic projection">Stereographic projection</a></li> <li><a href="/wiki/Strike_and_dip" title="Strike and dip">Strike and dip</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%">Large-scale <a href="/wiki/Tectonics" title="Tectonics">tectonics</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Accretionary_wedge" title="Accretionary wedge">Accretionary wedge</a></li> <li><a href="/wiki/Allochthon" title="Allochthon">Allochthon</a></li> <li><a href="/wiki/Autochthon_(geology)" title="Autochthon (geology)">Autochthon</a></li> <li><a href="/wiki/Back-arc_basin" title="Back-arc basin">Back-arc basin</a></li> <li><a href="/wiki/Continental_collision" title="Continental collision">Continental collision</a></li> <li><a href="/wiki/Convergent_boundary" title="Convergent boundary">Convergent boundary</a></li> <li><a href="/wiki/D%C3%A9collement" title="Décollement">Décollement</a></li> <li><a href="/wiki/Divergent_boundary" title="Divergent boundary">Divergent boundary</a></li> <li><a href="/wiki/Extensional_tectonics" title="Extensional tectonics">Extensional tectonics</a></li> <li><a href="/wiki/Fault_block" title="Fault block">Fault block</a></li> <li><a href="/wiki/Window_(geology)" title="Window (geology)">Fenster</a></li> <li><a href="/wiki/Fold_and_thrust_belt" title="Fold and thrust belt">Fold and thrust belt</a></li> <li><a href="/wiki/Fold_mountains" title="Fold mountains">Fold mountains</a></li> <li><a href="/wiki/Foreland_basin" title="Foreland basin">Foreland basin</a></li> <li><a href="/wiki/Graben" title="Graben">Graben</a></li> <li><a href="/wiki/Half-graben" title="Half-graben">Half-graben</a></li> <li><a href="/wiki/Horse_(geology)" title="Horse (geology)">Horse</a></li> <li><a href="/wiki/Horst_(geology)" title="Horst (geology)">Horst</a></li> <li><a href="/wiki/Horst_and_graben" title="Horst and graben">Horst and graben</a></li> <li><a href="/wiki/Intra-arc_basin" title="Intra-arc basin">Intra-arc basin</a></li> <li><a href="/wiki/Inversion_(geology)" title="Inversion (geology)">Inversion</a></li> <li><a href="/wiki/Klippe" title="Klippe">Klippe</a></li> <li><a href="/wiki/List_of_tectonic_plate_interactions" title="List of tectonic plate interactions">List of tectonic plate interactions</a></li> <li><a href="/wiki/M%C3%A9lange" title="Mélange">Mélange</a></li> <li><a href="/wiki/Mountain_formation" title="Mountain formation">Mountain formation</a></li> <li><a href="/wiki/Nappe" title="Nappe">Nappe</a></li> <li><a href="/wiki/Obduction" title="Obduction">Obduction</a></li> <li><a href="/wiki/Orogeny" title="Orogeny">Orogeny</a></li> <li><a href="/wiki/Passive_margin" title="Passive margin">Passive margin</a></li> <li><a href="/wiki/Plate_tectonics" title="Plate tectonics">Plate tectonics</a></li> <li><a href="/wiki/Pull-apart_basin" title="Pull-apart basin">Pull-apart basin</a></li> <li><a href="/wiki/Rift_valley" title="Rift valley">Rift valley</a></li> <li><a class="mw-selflink selflink">Rift</a></li> <li><a href="/wiki/Saddle_(landform)" title="Saddle (landform)">Saddle</a></li> <li><a href="/wiki/Strike-slip_tectonics" title="Strike-slip tectonics">Strike-slip tectonics</a></li> <li><a href="/wiki/Structural_basin" title="Structural basin">Structural basin</a></li> <li><a href="/wiki/Suture_(geology)" title="Suture (geology)">Suture</a></li> <li><a href="/wiki/Syneclise" class="mw-redirect" title="Syneclise">Syneclise</a></li> <li><a href="/wiki/Terrane" title="Terrane">Terrane</a></li> <li><a href="/wiki/Thick-skinned_deformation" title="Thick-skinned deformation">Thick-skinned deformation</a></li> <li><a href="/wiki/Thin-skinned_deformation" title="Thin-skinned deformation">Thin-skinned deformation</a></li> <li><a href="/wiki/Thrust_tectonics" title="Thrust tectonics">Thrust tectonics</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Fracture_(geology)" title="Fracture (geology)">Fracturing</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Columnar_jointing" title="Columnar jointing">Columnar jointing</a></li> <li><a href="/wiki/Dike_(geology)" title="Dike (geology)">Dike</a></li> <li><a href="/wiki/Exfoliation_joint" title="Exfoliation joint">Exfoliation joint</a></li> <li><a href="/wiki/Fissure" title="Fissure">Fissure</a></li> <li><a href="/wiki/Joint_(geology)" title="Joint (geology)">Joint</a></li> <li><a href="/wiki/Vein_(geology)" title="Vein (geology)">Vein</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Fault_(geology)" title="Fault (geology)">Faulting</a></th><td class="navbox-list-with-group navbox-list navbox-odd" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Asperity_(faults)" title="Asperity (faults)">Asperity</a></li> <li><a href="/wiki/Cataclasite" title="Cataclasite">Cataclasite</a></li> <li><a href="/wiki/Cataclastic_rock" title="Cataclastic rock">Cataclastic rock</a></li> <li><a href="/wiki/Detachment_fault" title="Detachment fault">Detachment fault</a></li> <li><a href="/wiki/Disturbance_(geology)" title="Disturbance (geology)">Disturbance</a></li> <li><a href="/wiki/Fault_friction" title="Fault friction">Fault friction</a></li> <li><a href="/wiki/Fault_mechanics" title="Fault mechanics">Fault mechanics</a></li> <li><a href="/wiki/Fault_scarp" title="Fault scarp">Fault scarp</a></li> <li><a href="/wiki/Fault_trace" title="Fault trace">Fault trace</a></li> <li><a href="/wiki/Thrust_fault" title="Thrust fault">Thrust fault</a></li> <li><a href="/wiki/Transfer_zone" title="Transfer zone">Transfer zone</a></li> <li><a href="/wiki/Transform_fault" title="Transform fault">Transform fault</a></li></ul> </div></td></tr><tr><th scope="row" class="navbox-group" style="width:1%"><a href="/wiki/Foliation_(geology)" title="Foliation (geology)">Foliation</a> and <a href="/wiki/Lineation_(geology)" title="Lineation (geology)">lineation</a></th><td class="navbox-list-with-group navbox-list navbox-even" style="width:100%;padding:0"><div style="padding:0 0.25em"> <ul><li><a href="/wiki/Cleavage_(geology)" title="Cleavage (geology)">Cleavage</a></li> <li><a href="/wiki/Compaction_(geology)" title="Compaction (geology)">Compaction</a></li> <li><a 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