GEOLOGIJA | Proleksis enciklopedija

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<li><a href="https://proleksis.lzmk.hr/tag/pravo-pravni-sustav-i-drzavno-uredenje/" class="tag-cloud-link tag-link-22 tag-link-position-18" style="font-size: 8pt;">PRAVO – PRAVNI SUSTAV I DRŽAVNO UREĐENJE</a></li> <li><a href="https://proleksis.lzmk.hr/tag/tehnika-i-tehnicke-znanosti/" class="tag-cloud-link tag-link-9 tag-link-position-19" style="font-size: 8pt;">TEHNIKA I TEHNIČKE ZNANOSTI</a></li> <li><a href="https://proleksis.lzmk.hr/tag/vojnistvo/" class="tag-cloud-link tag-link-15 tag-link-position-20" style="font-size: 8pt;">VOJNIŠTVO</a></li> <li><a href="https://proleksis.lzmk.hr/tag/sport-igre-i-rekreacija/" class="tag-cloud-link tag-link-16 tag-link-position-21" style="font-size: 8pt;">ŠPORT – IGRE I REKREACIJA</a></li> </ul> </div> </div></div></div> </div> </div> <div id="toppose" class="tpPose">  </div> </div> <div id="container" class="pe-layout-cell pe-content clearfix"> <div class="pe-post pe-article breadcrumbs"> <div class="pe-postcontent clearfix"><h4 class="box-title">GEOLOGIJA</h4></div> </div> <div class="pe-post pe-article "> <div class="pe-postcontent clearfix"> <div id='wp_page_numbers'> <ul><li class="active_page"><a href="https://proleksis.lzmk.hr/tag/geologija/">1</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/2/">2</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/3/">3</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/4/">4</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/5/">5</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/6/">6</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/7/">7</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/8/">8</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/9/">9</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/10/">10</a></li> <li class="space"></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/34/">»</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/2/">&rsaquo;</a></li> </ul> <div style='float: none; clear: both;'></div> </div> </div> </div> <div id="post-6509" class="pe-post pe-article post-6509 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/6509/" rel="bookmark" title="aa lava">aa lava</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <a title="aa lava na Havajima" href="https://proleksis.lzmk.hr/slike/x_a0234.JPG" class="broken_link"> </a></p> <span class="Natuknica">aa lava</span><span class="Normal">, tip lave, odnosno ohlađena lava koja oblikuje neravnu, nazubljenu površinu izrazitih bridova. Nastaje kada plinovi i tekuća lava probijaju i kidaju već skrutnutu koru. Hlađenjem nastaju crni, oštrobridni blokovi. </span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="12:24">23. listopada 2013.</span></span></div> </div> <div id="post-6655" class="pe-post pe-article post-6655 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/6655/" rel="bookmark" title="abisalni sedimenti">abisalni sedimenti</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>abisalni sedimenti</b></span><span class="Normal">, sedimenti dubokog mora, razlikuju se različite vrste mulja među recentnim sedimentima: hemipelagički (plavi, crveni, zeleni) i eupelagički (globigerinski, kokolitoforidni, pte-ropodni, crvena glina, radiolarijski, dijatomejski) muljevi.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-6658" class="pe-post pe-article post-6658 post type-post status-publish format-standard hentry tag-bioloske-i-medicinske-znanosti-i-podrucja tag-geologija tag-tehnika-i-tehnicke-znanosti"> <h1 class="pe-postheader"><span class="pe-postheadericon_bl pe-postheadericon_more" id="https://proleksis.lzmk.hr/6658/"></span><a href="https://proleksis.lzmk.hr/6658/" rel="bookmark" title="ablacija">ablacija</a></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/bioloske-i-medicinske-znanosti-i-podrucja/" rel="tag">BIOLOŠKE I MEDICINSKE ZNANOSTI I PODRUČJA</a>, <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a>, <a href="https://proleksis.lzmk.hr/tag/tehnika-i-tehnicke-znanosti/" rel="tag">TEHNIKA I TEHNIČKE ZNANOSTI</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>ablacija </strong></span><span class="Normal">(latinski: <em>ablatio</em>) 1. Odnošenje površinskih slojeva zemlje zbog djelovanja erozije i otapanje i isparivanje leda s površine ledenjaka. 2. <em>med</em> Operativno odstranjenje organa i njihovih dijelova (na primjer dojke) ili odljepljenje jednog tkiva od drugoga (na primjer mrežnice… <a class="more-link" href="https://proleksis.lzmk.hr/6658/">Nastavi čitati <span class="meta-nav">→</span></a></span></div> <div id="loaderer_post-6658" style="display:none"><div class="loaderGif"></div></div><div class="pe-postcontent clearfix" style="display:none" id="full_content_post-6658"></div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="06:32">14. veljače 2013.</span></span></div> </div> <div id="post-6698" class="pe-post pe-article post-6698 post type-post status-publish format-standard hentry tag-bioloske-i-medicinske-znanosti-i-podrucja tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon_bl pe-postheadericon_more" id="https://proleksis.lzmk.hr/6698/"></span><a href="https://proleksis.lzmk.hr/6698/" rel="bookmark" title="abrazija">abrazija</a></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/bioloske-i-medicinske-znanosti-i-podrucja/" rel="tag">BIOLOŠKE I MEDICINSKE ZNANOSTI I PODRUČJA</a>, <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>abrazija</strong></span><span class="Normal"> (latinski <em>abrado: </em>ostrugati) 1. <em>med</em> Površinsko oštećenje nekog organa, na primjer kože, zuba; operativno struganje površinskog epitela kože i sluznice, na primjer dermoabrazija za uklanjanje ožiljaka i tetovaže, abrazija maternice (kiretaža), abrazija rožnice (kod herpetičnoga keratitisa). 2.… <a class="more-link" href="https://proleksis.lzmk.hr/6698/">Nastavi čitati <span class="meta-nav">→</span></a></span></div> <div id="loaderer_post-6698" style="display:none"><div class="loaderGif"></div></div><div class="pe-postcontent clearfix" style="display:none" id="full_content_post-6698"></div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="10:58">15. veljače 2013.</span></span></div> </div> <div id="post-6727" class="pe-post pe-article post-6727 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/6727/" rel="bookmark" title="abukuma">abukuma</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>abukuma</b></span><span class="Normal">, serija metamorfnih facijesa, karakterizirana je slijedom metamorfnih facijesa niskog tlaka, od zeolitnog do granulitnog facijesa, koji nastaju metamorfozom uz geotermalni gradijent od 40–80°/km i progresiju andaluzita i silimanita.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-47300" class="pe-post pe-article post-47300 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/47300/" rel="bookmark" title="ACF-dijagram">ACF-dijagram</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>ACF-dijagram</strong></span><span class="Normal">, trokomponentni dijagram koji pokazuje kemijski karakter stijene; koristi se kod metamorfnih stijena, A=Al</span><sub>2</sub><span class="Normal">O</span><sub>3</sub><span class="Normal">+Fe</span><sub>2</sub><span class="Normal">O</span><sub>3</sub><span class="Normal">-(Na</span><sub>2</sub><span class="Normal">O+K</span><sub>2</sub><span class="Normal">O), C=CaO, F=FeO+MgO+MnO.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="14:34">18. veljače 2013.</span></span></div> </div> <div id="post-4995" class="pe-post pe-article post-4995 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/4995/" rel="bookmark" title="adamelit">adamelit</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>adamelit</b></span><span class="Normal">, kisela magmatska intruzivna (dubinska) stijena, sastoji se od kvarca, K-feldspata i plagioklasa; sinonim za kvarc-monzonit.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-6947" class="pe-post pe-article post-6947 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/6947/" rel="bookmark" title="Adria">Adria</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>Adria</strong></span><span class="Normal">, litosferni kontinentalni blok predgorja afričkoga kratona. Naziva se i Apulijskom pločom i Jadranskom pločom (u hrvatskom geološkom nazivlju). </span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="14:25">22. veljače 2013.</span></span></div> </div> <div id="post-6959" class="pe-post pe-article post-6959 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/6959/" rel="bookmark" title="adular">adular</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>adular</strong></span><span class="Normal"> (od Mons Adula, u švicarskim Alpama), bezbojan do bjelkast mineral hidrotermalnog postanka, varijetet ortoklasa; ukrasni mineral.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="14:30">22. veljače 2013.</span></span></div> </div> <div id="post-7009" class="pe-post pe-article post-7009 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/7009/" rel="bookmark" title="aerolit">aerolit</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>aerolit</strong></span><span class="Normal"> (grčki), kameni meteorit sastavljen od kisika, željeza, silicija i magnezija. Od svih meteorita 95% su aeroliti. </span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="11:00">26. veljače 2013.</span></span></div> </div> <div id="post-7037" class="pe-post pe-article post-7037 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/7037/" rel="bookmark" title="afanitska struktura">afanitska struktura</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>afanitska struktura</b></span><span class="Normal">, struktura magmatskih stijena kod kojih su minerali tako sitni da se ne razlikuju golim okom.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-5066" class="pe-post pe-article post-5066 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/5066/" rel="bookmark" title="aglomerat">aglomerat</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>aglomerat</b></span><span class="Normal">, nakupina međusobno povezanih materijala; kod piroklastičnih stijena sastoji se od</span><span class="Normal"> vulkanskih bombi.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-7127" class="pe-post pe-article post-7127 post type-post status-publish format-standard hentry tag-geologija tag-tehnika-i-tehnicke-znanosti"> <h1 class="pe-postheader"><span class="pe-postheadericon_bl pe-postheadericon_more" id="https://proleksis.lzmk.hr/7127/"></span><a href="https://proleksis.lzmk.hr/7127/" rel="bookmark" title="agregat">agregat</a></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a>, <a href="https://proleksis.lzmk.hr/tag/tehnika-i-tehnicke-znanosti/" rel="tag">TEHNIKA I TEHNIČKE ZNANOSTI</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><strong>agregat </strong></span><span class="Normal">(latinski) 1. Nešto što je složeno, od različitih dijelova sastavljeno u jedno. 2. <em>tehn</em> Skupina istovrsnih ili raznovrsnih dijelova koji zajedno čine jedinicu ili radnu cjelinu (uređaj), npr. parna turbina, motor s unutarnjim izgaranjem, električni generator. 3. <em>građev</em> Mineralni… <a class="more-link" href="https://proleksis.lzmk.hr/7127/">Nastavi čitati <span class="meta-nav">→</span></a></span></div> <div id="loaderer_post-7127" style="display:none"><div class="loaderGif"></div></div><div class="pe-postcontent clearfix" style="display:none" id="full_content_post-7127"></div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="11:54">1. ožujka 2013.</span></span></div> </div> <div id="post-4920" class="pe-post pe-article post-4920 post type-post status-publish format-standard hentry tag-geologija tag-licnosti"> <h1 class="pe-postheader"><span class="pe-postheadericon_bl pe-postheadericon_more" id="https://proleksis.lzmk.hr/4920/"></span><a href="https://proleksis.lzmk.hr/4920/" rel="bookmark" title="Agricola, Georgius">Agricola, Georgius</a></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a>, <a href="https://proleksis.lzmk.hr/tag/licnosti/" rel="tag">LIČNOSTI</a></span></div> <div class="pe-postcontent clearfix"> <a title="" href="https://proleksis.lzmk.hr/slike/x_a0262.JPG" class="broken_link"></a> <span class="Natuknica"><strong>Agricola, Georgius </strong></span><span class="Normal">(pravim imenom i prezimenom Georg Bauer), njemački filolog, prirodoslovac i liječnik (Glauchau, 24. III. 1494 – Chemnitz, 21. IX. 1555). Nazvan “ocem mineralogije”, osnivač rudarstva s metalurgijom kao znanošću. Prvi klasificirao minerale po fizikalnim… <a class="more-link" href="https://proleksis.lzmk.hr/4920/">Nastavi čitati <span class="meta-nav">→</span></a></span></div> <div id="loaderer_post-4920" style="display:none"><div class="loaderGif"></div></div><div class="pe-postcontent clearfix" style="display:none" id="full_content_post-4920"></div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="15:44">24. ožujka 2014.</span></span></div> </div> <div id="post-6475" class="pe-post pe-article post-6475 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/6475/" rel="bookmark" title="ahat">ahat</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <p><a title="" href="https://proleksis.lzmk.hr/slike/ahat.JPG" class="broken_link"></a></p> <span class="Natuknica"><b>ahat</b></span><span class="Normal"> (grčki: <em>Achátes,</em> grčko ime rijeke na Siciliji, danas Dirillo), sitnozrnati kremen, → <a href="https://proleksis.lzmk.hr/54598/" class="broken_link">kalcedon</a>, zonalne građe s različito obojenim zonama, kriptokristalni varijetet. Upotrebljava se kao ukrasni kamen i za izradu laboratorijskoga posuđa (ahatni tarionik).</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="12:34">11. ožujka 2016.</span></span></div> </div> <div id="post-7376" class="pe-post pe-article post-7376 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/7376/" rel="bookmark" title="ahondrit">ahondrit</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>ahondrit</b></span><span class="Normal">, kameni meteorit bez hondra.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-51528" class="pe-post pe-article post-51528 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/51528/" rel="bookmark" title="akadij">akadij</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>akadij</b></span><span class="Normal">, srednji → </span><a href="https://proleksis.lzmk.hr/?p=29808" class="broken_link"><span class="uputnica">kambrij</span></a><span class="Normal">.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-5154" class="pe-post pe-article post-5154 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/5154/" rel="bookmark" title="akantit">akantit</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>akantit</b></span><span class="Normal">, mineral, Ag<sub>2</sub>S, kristalizira u monoklinskom sustavu, stabilan u hidrotermalnim uvjetima ispod 179 °C. → </span><a href="https://proleksis.lzmk.hr/?p=9392" class="broken_link"><span class="uputnica">argentit</span></a> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div id="post-5155" class="pe-post pe-article post-5155 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/5155/" rel="bookmark" title="akantoceras">akantoceras</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <a title="" href="https://proleksis.lzmk.hr/slike/akantoceras.JPG" class="broken_link"></a></p> <span class="Natuknica"><strong>akantoceras</strong></span><span class="Normal"> <em>(Acanthoceras),</em> gornjokredni amonit.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Ažurirano:</span> <span class="entry-date" title="11:47">8. ožujka 2013.</span></span></div> </div> <div id="post-5175" class="pe-post pe-article post-5175 post type-post status-publish format-standard hentry tag-geologija"> <h1 class="pe-postheader"><span class="pe-postheadericon"><a href="https://proleksis.lzmk.hr/5175/" rel="bookmark" title="akcesorni minerali">akcesorni minerali</a></span></h1> <div class="pe-postheadericons pe-metadata-icons"><span class="pe-posttagicon"><span class="tags">Struka</span> <a href="https://proleksis.lzmk.hr/tag/geologija/" rel="tag">GEOLOGIJA</a></span></div> <div class="pe-postcontent clearfix"> <span class="Natuknica"><b>akcesorni minerali</b></span><span class="Normal">, minerali koji se javljaju u bilo kojoj skupini stijena (magmatskoj, sedimentnoj ili metamorfnoj) i dolaze u razmjerno malim količinama (do 1%). U sedimentnim stijenama oni su sinonim za → </span><a href="https://proleksis.lzmk.hr/?p=54393" class="broken_link"><span class="uputnica">teške minerale</span></a><span class="Normal">.</span> </div> <div class="pe-postfootericons pe-metadata-icons"><span class="pe-postdateicon"><span class="date">Objavljeno:</span> <span class="entry-date" title="15:59">22. lipnja 2012.</span></span></div> </div> <div class="pe-post pe-article "> <div class="pe-postcontent clearfix"> <div id='wp_page_numbers'> <ul><li class="active_page"><a href="https://proleksis.lzmk.hr/tag/geologija/">1</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/2/">2</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/3/">3</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/4/">4</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/5/">5</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/6/">6</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/7/">7</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/8/">8</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/9/">9</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/10/">10</a></li> <li class="space"></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/34/">»</a></li> <li class="first_last_page"><a href="https://proleksis.lzmk.hr/tag/geologija/page/2/">&rsaquo;</a></li> </ul> <div style='float: none; clear: both;'></div> </div> </div> </div> </div> </div> </div> </div> <footer class="pe-footer clearfix"> <div class="pe-footer-inner"> <div class="pe-content-layout"> <div class="pe-content-layout-row"> <div class="pe-layout-cell layout-item-0" style="width: 100%">  <div style="position:relative;padding-left:10px;padding-right:10px"> <p>Copyright © 2013. <a href="http://www.lzmk.hr/">Leksikografski zavod Miroslav Krleža</a>. 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