{"id":44212,"date":"2024-11-04T07:22:12","date_gmt":"2024-11-04T07:22:12","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=44212"},"modified":"2024-11-04T07:44:41","modified_gmt":"2024-11-04T07:44:41","slug":"spread-and-frequency-of-explosive-silicic-volcanism-of-the-carpathian-pannonian-region-during-early-miocene-clues-from-the-sw-pannonian-basin-and-the-dinarides","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/spread-and-frequency-of-explosive-silicic-volcanism-of-the-carpathian-pannonian-region-during-early-miocene-clues-from-the-sw-pannonian-basin-and-the-dinarides\/","title":{"rendered":"Spread and frequency of explosive silicic volcanism of the Carpathian-Pannonian Region during Early Miocene: Clues from the SW Pannonian Basin 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;4.27.2&#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; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\"><strong>Spread and frequency of explosive silicic volcanism of the Carpathian-Pannonian Region during Early Miocene: Clues from the SW Pannonian Basin and the Dinarides<\/strong><\/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\/2024\/11\/volcanology.jpg&#8221; alt=&#8221;Geosciences logo&#8221; title_text=&#8221;volcanology&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.27.2&#8243; width=&#8221;20%&#8221; max_width=&#8221;65%&#8221; module_alignment=&#8221;center&#8221; 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;][\/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;4.27.2&#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\u00a0<em>Journal of Volcanology and Geothermal Research\u00a0<\/em>objavljen je znanstveni rad pod naslovom\u00a0<strong><em>Spread and frequency of explosive silicic volcanism of the Carpathian-Pannonian Region during Early Miocene: Clues from the SW Pannonian Basin and the Dinarides<\/em><\/strong>. Rad je rezultat suradnje znanstvenika iz Hrvatskog geolo\u0161kog instituta te iz brojnih drugih institucija iz Hrvatske i inozemstva.<\/p>\n<p>U radu su prikazani rezultati integriranih analiza donjomiocenskih vulkanoklasti\u010dnih naslaga starih pribli\u017eno 17.3, 17.1 i 17 milijuna godina s podru\u010dja Kalni\u010dkog vulkanoklasti\u010dnog kompleksa (jugozapadni dio Panonskog bazena), Sinjskog i Livno-Tomislavgrad bazena (Dinaridski jezerski sustav), koji su korelirani s vulkanoklasti\u010dnim naslagama sjevernog dijela Panonskog bazena. Novi podatci upu\u0107uju da je u\u010destalost, ra\u0161irenost i veli\u010dina eksplozivnih silicijskih erupcija Karpatsko-panonske regije, koja predstavlja izvori\u0161te istra\u017eivanih vulkanoklasti\u010dnih horizonata, bila ve\u0107a tijekom donjeg miocena nego \u0161to je to ranije prepoznato.<\/p>\n<p>Istra\u017eivanje je provedeno u okviru projekta Hrvatske zaklade za znanost \u201eMiocenska sin-riftna evolucija Sjevernohrvatskog bazena (Karpatsko-Panonska regija): \u201cmulti-proxy\u201d pristup, korelacija i integriranje sedimentnog i vulkanskog zapisa\u201c akronima PYROSKA (HRZZ-UIP-2019-04-7761) voditelja dr.sc. Mihovila Brleka.<\/p>\n<p>Rad je dostupan na poveznicama:<\/p>\n<p><u><em><\/em><\/u><em><a href=\"https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0377027324002087?via%3Dihub;\">https:\/\/www.sciencedirect.com\/science\/article\/abs\/pii\/S0377027324002087?via%3Dihub;<\/a><\/em><\/p>\n<p><u><\/u><\/p>\n<p><em><a href=\"https:\/\/authors.elsevier.com\/a\/1k1Hp1LkU3jxyd\"><u>https:\/\/authors.elsevier.com\/a\/1k1Hp1LkU3jxyd<\/u><\/a><\/em><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>NAJNOVIJI OBJAVLJENI RADOVISpread and frequency of explosive silicic volcanism of the Carpathian-Pannonian Region during Early Miocene: Clues from the SW Pannonian Basin and the DinaridesU znanstvenom \u010dasopisu\u00a0Journal of Volcanology and Geothermal Research\u00a0objavljen je znanstveni rad pod naslovom\u00a0Spread and frequency of explosive silicic volcanism of the Carpathian-Pannonian Region during Early Miocene: Clues from the SW Pannonian [&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-44212","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/44212","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=44212"}],"version-history":[{"count":4,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/44212\/revisions"}],"predecessor-version":[{"id":44223,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/44212\/revisions\/44223"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=44212"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}