{"id":42589,"date":"2023-10-17T09:41:30","date_gmt":"2023-10-17T09:41:30","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=42589"},"modified":"2023-10-17T09:51:26","modified_gmt":"2023-10-17T09:51:26","slug":"provenance-and-depositional-environment-of-middle-miocene-silicic-volcaniclastic-deposits-from-mt-medvednica-north-croatian-basin-carpathian-pannonian-region","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/provenance-and-depositional-environment-of-middle-miocene-silicic-volcaniclastic-deposits-from-mt-medvednica-north-croatian-basin-carpathian-pannonian-region\/","title":{"rendered":"Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region)"},"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=”4.22.1″ 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

Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region)<\/strong>\u00a0<\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”20px||41px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ custom_padding=”0px|||||” 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_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/10\/journal.jpg” alt=”springer” title_text=”journal” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.22.2″ width=”30%” max_width=”35%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px|||||” 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=”4.22.2″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

U znanstvenom \u010dasopisu Journal of Volcanology and Geothermal Research <\/span><\/em>objavljen je znanstveni rad pod naslovom Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region)<\/i><\/b> Rad je rezultat suradnje znanstvenika iz Hrvatskog geolo\u0161kog instituta te iz brojnih drugih institucija iz Hrvatske i inozemstva.<\/o:p><\/p>\n

U radu su prikazani rezultati integriranog pristupa kori\u0161tenja vulkanolo\u0161kih, geokronolo\u0161kih i paleontolo\u0161kih analiza na vulkanoklasti\u010dnim naslaga s podru\u010dja Medvednice. Novi podatci visokoprecizne geokronologije na mineralu cirkonu te geokemije na vulkanskom staklu omogu\u0107ili su razlikovanje dva vulkanoklasti\u010dna horizonta \u201ePlaz\u201c i \u201eBidrovec\u201c koji su produkt dvije odvojene erupcije. Tefrostratigrafijom je povezan horizont \u201ePlaz\u201c s Demj\u00e9n erupcijom\u00a0 koja je definirana s debelim ignimbritskim naslagama na sjeveru Ma\u0111arske, dok horizont \u201eBidrovec\u201c nije mogu\u0107e povezati s ni jednom poznatom erupcijom. Ovi podatci \u0107e omogu\u0107iti primjenu horizonata \u201ePlaz\u201c i \u201eBidrovec\u201c kao va\u017enih marker horizonata za regionalne rekonstrukcije, te pomo\u0107i u boljem razumijevanju vulkanske kronologije i tefrostratigrafije Karpatsko-panonske regije.<\/o:p><\/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.<\/o:p><\/p>\n

Rad je dostupan na poveznici: https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0377027323001749<\/em><\/a><\/o:p><\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVIProvenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region)\u00a0U znanstvenom \u010dasopisu Journal of Volcanology and Geothermal Research objavljen je znanstveni rad pod naslovom Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region) Rad je rezultat […]<\/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-42589","page","type-page","status-publish","hentry"],"aioseo_notices":[],"aioseo_head":"\n\t\t\n\t\n\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t