{"id":39220,"date":"2021-04-30T08:08:25","date_gmt":"2021-04-30T08:08:25","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=39220"},"modified":"2021-04-30T08:13:21","modified_gmt":"2021-04-30T08:13:21","slug":"cenomanian-turonian-oceanic-anoxic-event-oae2-imprint-on-the-northwestern-part-of-the-adriatic-carbonate-platform-and-a-coeval-intra-platform-basin-istria-and-premuda-island-croatia","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/cenomanian-turonian-oceanic-anoxic-event-oae2-imprint-on-the-northwestern-part-of-the-adriatic-carbonate-platform-and-a-coeval-intra-platform-basin-istria-and-premuda-island-croatia\/","title":{"rendered":"Cenomanian\u2013Turonian Oceanic Anoxic Event (OAE2) imprint on the northwestern part of the Adriatic Carbonate Platform and a coeval intra-platform basin (Istria and Premuda Island, Croatia)"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.4.1″ custom_padding=”0px||0px|||”][et_pb_fullwidth_slider _builder_version=”4.4.2″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.6.6″ text_font_size=”32px” header_2_text_color=”#1e5096″]<\/p>\n

NAJNOVIJI OBJAVLJENI RADOVI<\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.9.4″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em” hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Cenomanian\u2013Turonian Oceanic Anoxic Event (OAE2) imprint on the northwestern part of the Adriatic Carbonate Platform and a coeval intra-platform basin (Istria and Premuda Island, Croatia)<\/span><\/h2>\n

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Znanstveni rad objavljen u \u010dasopisu Cretaceous Research rezultat je sedimentolo\u0161kih, paleontolo\u0161kih i geokemijskih istra\u017eivanja provedenih na podru\u010dju Istre (Barban) i otoka Premuda od strane geologa iz Hrvatskog geolo\u0161kog instituta i Smith Collegea iz Massachusettsa. Rad predstavlja doprinos na podru\u010dju definiranja okoli\u0161a i nastanka razli\u010ditih facijesa tijekom mla\u0111e krede (cenomana i turona) tada\u0161nje Jadranske karbonatne platforme. Naglasak je postavljen na utjecaj globalnog Oceanskog anoksi\u010dnog doga\u0111aja (OAE2) i preplavljivanja plitkovodne platforme tijekom prijelaza cenoman-turon. U radu su kori\u0161tene litolo\u0161ke, biolo\u0161ke i mikrofacijesne analize te SEM, EDS, TOC i analize stabilnih izotopa (\u03b413C i \u03b418O).<\/p>\n

Link za pristup radu: https:\/\/authors.elsevier.com\/sd\/article\/S0195-6671(21)00094-X<\/em><\/a><\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVICenomanian\u2013Turonian Oceanic Anoxic Event (OAE2) imprint on the northwestern part of the Adriatic Carbonate Platform and a coeval intra-platform basin (Istria and Premuda Island, Croatia)Znanstveni rad objavljen u \u010dasopisu Cretaceous Research rezultat je sedimentolo\u0161kih, paleontolo\u0161kih i geokemijskih istra\u017eivanja provedenih na podru\u010dju Istre (Barban) i otoka Premuda od strane geologa iz Hrvatskog geolo\u0161kog instituta […]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-39220","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39220","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/comments?post=39220"}],"version-history":[{"count":2,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39220\/revisions"}],"predecessor-version":[{"id":39224,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39220\/revisions\/39224"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=39220"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}