{"id":41975,"date":"2023-03-21T07:00:45","date_gmt":"2023-03-21T07:00:45","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=41975"},"modified":"2023-05-18T05:41:38","modified_gmt":"2023-05-18T05:41:38","slug":"biostratigraphy-and-facies-description-of-middle-triassi-rift-related-volcano-sedimentary-successions-at-the-junction-of-the-southern-alps-and-the-dinarides","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/biostratigraphy-and-facies-description-of-middle-triassi-rift-related-volcano-sedimentary-successions-at-the-junction-of-the-southern-alps-and-the-dinarides\/","title":{"rendered":"Biostratigraphy and facies description of Middle Triassi rift-related volcano-sedimentary successions at the junction of the Southern Alps and the Dinarides"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; fullwidth=&#8221;on&#8221; _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;0px||0px|||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_fullwidth_slider _builder_version=&#8221;4.16&#8243; 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global_colors_info=&#8221;{}&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.16&#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; global_colors_info=&#8221;{}&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.16&#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; global_colors_info=&#8221;{}&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.16&#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; global_colors_info=&#8221;{}&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.16&#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; global_colors_info=&#8221;{}&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.16&#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; global_colors_info=&#8221;{}&#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;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_row _builder_version=&#8221;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.16&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243; global_colors_info=&#8221;{}&#8221;]<\/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;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.19.4&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243; header_2_line_height=&#8221;1.3em&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\">Biostratigraphy and facies description of Middle Triassi rift-related volcano-sedimentary successions at the junction of the Southern Alps and the Dinarides<\/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;4.16&#8243; custom_padding=&#8221;20px||41px|||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row _builder_version=&#8221;4.16&#8243; custom_padding=&#8221;0px|||||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_image src=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/05\/earth-science.jpg&#8221; alt=&#8221;springer&#8221; title_text=&#8221;earth science&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.20.4&#8243; width=&#8221;36%&#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; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.16&#8243; min_height=&#8221;192px&#8221; custom_margin=&#8221;12px|auto||auto||&#8221; custom_padding=&#8221;0px|||||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.19.4&#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; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p>U znanstvenom \u010dasopisu <em>International Journal of Earth Sciences<\/em> <em>objavljen je znanstveni rad <\/em><em>Biostratigraphy and facies description of Middle Triassi rift-related volcano-sedimentary successions at the junction of the Southern Alps and the Dinarides.<\/em> U radu su opisane vulkano-sedimentne sukcesije srednjeg trijasa povezane s otvaranje Neotetis oceana. Intenzivna tektonska aktivnost povezana s riftovanjem dovela je u ovo vrijeme do regionalne diferencijacije talo\u017enih okoli\u0161a. Efuzivne i vulkanoklasti\u010dne stijene, koje u svom sastavu variraju od bazi\u010dnih do kiselih, talo\u017eene su u dubokomorskom okoli\u0161u, te se proslojavaju s pelagi\u010dkim vapnencima i ro\u017enjacima. Na istovremeno postojanje plitkomorskog talo\u017enog okoli\u0161a ukazuje pretalo\u017eeni karbonatni detritus. Podmorske efuzije bazalta i nastanak bazaltnih hijaloklastita povezani su s dubokim rasjedima koji su nastali uslijed ekstenzije. Kisele vulkanoklasti\u010dne stijene nastale su eksplozivnim vulkanskim erupcijama te su talo\u017eene u dubokomorskom okoli\u0161u razli\u010ditim gravitacijskim mehanizmima. Opisane sukcesije datirane su biostratigrafski amonitima, radiolarijama i benti\u010dkim foraminferama.\u00a0<\/p>\n<p>Istra\u017eivanje je provedeno u okviru projekta Hrvatske zaklade za znanost \u201eVulkano-sedimentne sukcesije sjeverozapadne Hrvatske i njihova uloga u razumijevanju geodinamike Paleotetisa tijekom srednjeg Trijasa\u201c akronima GOST (IP-2019-04-3824).<\/p>\n<p>Rad je dostupan na slijede\u0107oj poveznici: <a href=\"https:\/\/link.springer.com\/article\/10.1007\/s00531-023-02301-w\"><em>https:\/\/link.springer.com\/article\/10.1007\/s00531-023-02301-w<\/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 RADOVIBiostratigraphy and facies description of Middle Triassi rift-related volcano-sedimentary successions at the junction of the Southern Alps and the DinaridesU znanstvenom \u010dasopisu International Journal of Earth Sciences objavljen je znanstveni rad Biostratigraphy and facies description of Middle Triassi rift-related volcano-sedimentary successions at the junction of the Southern Alps and the Dinarides. U radu [&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-41975","page","type-page","status-publish","hentry"],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 4.9.9 - aioseo.com -->\n\t<meta name=\"robots\" content=\"max-image-preview:large\" \/>\n\t<link rel=\"canonical\" href=\"https:\/\/www.hgi-cgs.hr\/en\/biostratigraphy-and-facies-description-of-middle-triassi-rift-related-volcano-sedimentary-successions-at-the-junction-of-the-southern-alps-and-the-dinarides\/\" \/>\n\t<meta name=\"generator\" content=\"All in One SEO (AIOSEO) 4.9.9\" \/>\n\t\t<meta property=\"og:locale\" content=\"en_US\" \/>\n\t\t<meta property=\"og:site_name\" content=\"Hrvatski geolo\u0161ki institut |\" \/>\n\t\t<meta property=\"og:type\" content=\"article\" \/>\n\t\t<meta 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