{"id":43951,"date":"2024-08-20T10:46:24","date_gmt":"2024-08-20T10:46:24","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=43951"},"modified":"2024-08-20T10:50:10","modified_gmt":"2024-08-20T10:50:10","slug":"a-distal-record-of-the-middle-miocene-silicic-eruption-of-the-carpathian-pannonian-region-stored-within-the-dinaride-lake-system-implications-for-tephrostratigraphy-and-emplacement-of-volcaniclastic","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/a-distal-record-of-the-middle-miocene-silicic-eruption-of-the-carpathian-pannonian-region-stored-within-the-dinaride-lake-system-implications-for-tephrostratigraphy-and-emplacement-of-volcaniclastic\/","title":{"rendered":"A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the Dinaride Lake System: implications for tephrostratigraphy and emplacement of volcaniclastic deposits"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_fullwidth_slider _builder_version=”4.16″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ 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” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ 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” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ 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” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” global_colors_info=”{}” sticky_transition=”on” theme_builder_area=”post_content”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.16″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

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

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.0″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

\u00a0A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the Dinaride Lake System: implications for tephrostratigraphy and emplacement of volcaniclastic deposits<\/strong><\/em><\/span><\/h2>\n

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U znanstvenom \u010dasopisu\u00a0International Journal of Earth Sciences\u00a0<\/em>objavljen je znanstveni rad pod naslovom\u00a0A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the Dinaride Lake System: implications for tephrostratigraphy and emplacement of volcaniclastic deposits<\/em><\/strong>. Rad je rezultat suradnje znanstvenika iz Hrvatskog geolo\u0161kog instituta te iz brojnih drugih institucija iz Hrvatske i inozemstva.<\/p>\n

U radu su prikazani rezultati integriranih analiza srednjomiocenskih vulkanoklasti\u010dnih naslaga s podru\u010dja Livno-Tomislavgrad bazena (Dinaridski jezerski sustav). Novi podatci upu\u0107uju da je u\u010destalost eksplozivnih silicijskih erupcija Karpatsko-panonske regije, koja predstavlja izvori\u0161te istra\u017eivanih Dinaridskih vulkanoklasti\u010dnih horizonata, bila ve\u0107a tijekom srednjeg miocena nego \u0161to je to ranije prepoznato. Tako\u0111er, predlo\u017een je i model talo\u017eenja vulkanoklasti\u010dnih naslaga starih ~14.32 milijuna godina. Iako istra\u017eivane vulkanoklasti\u010dne naslage predstavljaju pouzdan tefro- i tektono-stratigrafski marker, ovo istra\u017eivanje upu\u0107uje na va\u017enost prepoznavanja sekundarnog sedimentacijskog zadebljanja tefre u distalnim (npr. jezerskim) okoli\u0161ima, po\u0161to se takve naslage ne mogu koristiti pri procjenama ukupnog volumena eruptirane tefre proizvedene eksplozivnim erupcijama.<\/p>\n

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

Rad je dostupan na poveznicama:<\/p>\n

https:\/\/link.springer.com\/journal\/531<\/a><\/em>,<\/p>\n

https:\/\/rdcu.be\/dQ4sy<\/a><\/em>.<\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVI\u00a0A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the Dinaride Lake System: implications for tephrostratigraphy and emplacement of volcaniclastic depositsU znanstvenom \u010dasopisu\u00a0International Journal of Earth Sciences\u00a0objavljen je znanstveni rad pod naslovom\u00a0A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the […]<\/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-43951","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/43951","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=43951"}],"version-history":[{"count":3,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/43951\/revisions"}],"predecessor-version":[{"id":43955,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/43951\/revisions\/43955"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=43951"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}