{"id":38069,"date":"2021-01-11T08:56:00","date_gmt":"2021-01-11T08:56:00","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=38069"},"modified":"2021-01-11T08:58:46","modified_gmt":"2021-01-11T08:58:46","slug":"an-ensialic-volcanic-arc-along-the-northwestern-edge-of-palaeotethys-insights-from-the-mid%e2%80%90triassic-volcano%e2%80%90sedimentary-succession-of-ivanscica-mt-northwestern-croatia","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/an-ensialic-volcanic-arc-along-the-northwestern-edge-of-palaeotethys-insights-from-the-mid%e2%80%90triassic-volcano%e2%80%90sedimentary-succession-of-ivanscica-mt-northwestern-croatia\/","title":{"rendered":"An ensialic volcanic arc along the northwestern edge of Palaeotethys\u2014Insights from the Mid\u2010Triassic volcano\u2010sedimentary succession of Ivan\u0161\u010dica Mt. (northwestern Croatia)"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; fullwidth=&#8221;on&#8221; _builder_version=&#8221;4.4.1&#8243; custom_padding=&#8221;0px||0px|||&#8221;][et_pb_fullwidth_slider _builder_version=&#8221;4.4.2&#8243; min_height=&#8221;112px&#8221; height=&#8221;400px&#8221; custom_margin=&#8221;0px||||false|false&#8221; custom_padding=&#8221;0px||18px||false|false&#8221; auto=&#8221;on&#8221; auto_ignore_hover=&#8221;on&#8221; locked=&#8221;off&#8221;][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_row _builder_version=&#8221;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.6.6&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\"><strong>NAJNOVIJI OBJAVLJENI RADOVI<\/strong><\/h2>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.7.7&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243; header_2_line_height=&#8221;1.3em&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\">An ensialic volcanic arc along the northwestern edge of Palaeotethys\u2014Insights from the Mid\u2010Triassic volcano\u2010sedimentary succession of Ivan\u0161\u010dica Mt. (northwestern Croatia)<\/h2>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.4.2&#8243; custom_padding=&#8221;20px||41px|||&#8221;][et_pb_row _builder_version=&#8221;4.4.2&#8243; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_image src=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2021\/01\/2.-Geological-Journal_logo.jpg&#8221; title_text=&#8221;2. Geological Journal_logo&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.7.7&#8243; width=&#8221;100%&#8221; max_width=&#8221;35%&#8221; module_alignment=&#8221;center&#8221; hover_enabled=&#8221;0&#8243; border_radii=&#8221;on|5px|5px|5px|5px&#8221; box_shadow_style=&#8221;preset1&#8243; box_shadow_blur=&#8221;15px&#8221; sticky_enabled=&#8221;0&#8243;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.0.3&#8243; min_height=&#8221;192px&#8221; custom_margin=&#8221;12px|auto||auto||&#8221; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.0.3&#8243;][et_pb_text _builder_version=&#8221;4.7.7&#8243; text_font=&#8221;||||||||&#8221; link_font=&#8221;||||||||&#8221; link_text_color=&#8221;#e09900&#8243; custom_margin=&#8221;18px|||||&#8221; custom_padding=&#8221;|10px||10px|false|true&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p>Multidisciplinarna istra\u017eivanja u koja su osim znanstvenika iz HGI-a (Damir Slovenec, Josip Halami\u0107) bili uklju\u010deni i znanstvenici Branimir \u0160egvi\u0107 i Giovanni Zanoni iz Texas Tech University (USA), te \u0160pela Gori\u010dan iz Ivan Rakovec Institute of Paleontology (Slovenia) rezultirala su objavljivanjem znanstvenog rada naslova \u201cAn ensialic volcanic arc along the northwestern edge of Paleotethys \u2013 insights from the Mid-Triassic volcano-sedimentary succession of Ivan\u0161\u010dica Mt. (northwestern Croatia)\u201d u \u010dasopisu Geological Journal.<\/p>\n<p>Rezultati istra\u017eivanja razotkrivaju podrijetlo, geodinamske zna\u010dajke i dijagenetsku povijest piroklasti\u010dnih stijena i s njima udru\u017eenih radiolarijskih ro\u017enjaka dokumentiranih u srednjotrijaskoj (gornjoanizi\u010dkoj) vulkano-sedimentnoj sukcesiji koja izdanjuje na gori Ivan\u0161\u010dici u sjeverozapadnoj Hrvatskoj. Indicirana je polifazna eksplozivna vulkanska aktivnost i dubokomorska sedimentacija illirske starosti du\u017e ruba oceanskog podru\u010dja u okoli\u0161u smje\u0161tenom iznad supra-subdukcijske zone. To ide u prilog geodinamskoj evoluciji koja pretpostavlja postojanje aktivnog, ensiali\u010dnog i zrelog vulkanskog luka razvijenog du\u017e ju\u017enih aktivnih kontinentalnih rubova Laurussije tijekom gornjoanizi\u010dke subdukcije litosfere Paleotetisa.<\/p>\n<p>Rad je dostupan na poveznici: <a href=\"https:\/\/onlinelibrary.wiley.com\/doi\/10.1002\/gj.3664\"><em><a>https:\/\/onlinelibrary.wiley.com\/doi\/10.1002\/gj.3664<\/a> .<\/em><\/a><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>NAJNOVIJI OBJAVLJENI RADOVIAn ensialic volcanic arc along the northwestern edge of Palaeotethys\u2014Insights from the Mid\u2010Triassic volcano\u2010sedimentary succession of Ivan\u0161\u010dica Mt. (northwestern Croatia) Multidisciplinarna istra\u017eivanja u koja su osim znanstvenika iz HGI-a (Damir Slovenec, Josip Halami\u0107) bili uklju\u010deni i znanstvenici Branimir \u0160egvi\u0107 i Giovanni Zanoni iz Texas Tech University (USA), te \u0160pela Gori\u010dan iz Ivan Rakovec [&hellip;]<\/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-38069","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/38069","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=38069"}],"version-history":[{"count":2,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/38069\/revisions"}],"predecessor-version":[{"id":38073,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/38069\/revisions\/38073"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=38069"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}