{"id":39016,"date":"2021-03-16T13:31:03","date_gmt":"2021-03-16T13:31:03","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=39016"},"modified":"2021-03-16T13:56:58","modified_gmt":"2021-03-16T13:56:58","slug":"middle-triassic-high-k-calc-alkaline-effusive-and-pyroclastic-rocks-from-the-zagorje-mid-transdanubian-zone-mt-kuna-gora-nw-croatia-mineralogy-petrology-geochemistry-and-tectonomagmatic-affinit","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/middle-triassic-high-k-calc-alkaline-effusive-and-pyroclastic-rocks-from-the-zagorje-mid-transdanubian-zone-mt-kuna-gora-nw-croatia-mineralogy-petrology-geochemistry-and-tectonomagmatic-affinit\/","title":{"rendered":"Middle Triassic high-K calc-alkaline effusive and pyroclastic rocks from the Zagorje-Mid-Transdanubian Zone (Mt. Kuna Gora; NW Croatia): mineralogy, petrology, geochemistry and tectonomagmatic affinity"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.4.1″ custom_padding=”0px||0px|||”][et_pb_fullwidth_slider _builder_version=”4.4.2″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.6.6″ text_font_size=”32px” header_2_text_color=”#1e5096″]<\/p>\n

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

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.9.2″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em”]<\/p>\n

Middle Triassic high-K calc-alkaline effusive and pyroclastic rocks from the Zagorje-Mid-Transdanubian Zone (Mt. Kuna Gora; NW Croatia): mineralogy, petrology, geochemistry and tectonomagmatic affinity<\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″ custom_padding=”20px||41px|||”][et_pb_row _builder_version=”4.4.2″ custom_padding=”0px|||||”][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2021\/03\/Geologica-Acta_Logo.jpg” title_text=”Geologica Acta_Logo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.9.2″ width=”100%” max_width=”100%” module_alignment=”center” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.0.3″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px|||||”][et_pb_column type=”4_4″ _builder_version=”4.0.3″][et_pb_text _builder_version=”4.9.2″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true” hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Rezultati istra\u017eivanja u okviru projekta GOST (IP-2019-04-3824) Hrvatske zaklade za znanost objavljeni u \u010dasopisu Geologica Acta prikazuju prve detaljne mineralo\u0161ke, petrolo\u0161ke, geokemijske i izotopne podatke uklju\u010duju\u0107i i K-Ar starost (gornji anizik-donji ladinik) visoko-kalijskih kalcijsko-alkalijskih lava i s njima udru\u017eenih piroklasti\u010dnih stijena Kuna gore (SZ Hrvatska) smje\u0161tenoj u najju\u017enijem segmentu geotektonske jedinice Ju\u017enih Alpa odnosno jugozapadnom dijelu Zagorje-Srednje-Transdanubijske zone. Podaci ukazuju na kompleksno magmatsko podrijetlo taljevina generiranih na oko 50 km dubine i pri tlakovima od \u22641,6 GPa. Nastanak efuzivnih i piroklasti\u010dnih stijena povezan je sa sjevernovergentnom subdukcijom Paleotetiske oceanske litosfere u aktivnom ensiali\u010dnom zrelom vulkanskom luku smje\u0161tenom du\u017e ju\u017enog aktivnog kontinentalnog ruba Laurussije tijekom razdoblja ranog do srednjeg trijasa.<\/p>\n

Rad je dostupan na poveznici: <\/em><\/a>https:\/\/revistes.ub.edu\/index.php\/GEOACTA\/article\/view\/32053<\/a> .<\/em><\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVIMiddle Triassic high-K calc-alkaline effusive and pyroclastic rocks from the Zagorje-Mid-Transdanubian Zone (Mt. Kuna Gora; NW Croatia): mineralogy, petrology, geochemistry and tectonomagmatic affinityRezultati istra\u017eivanja u okviru projekta GOST (IP-2019-04-3824) Hrvatske zaklade za znanost objavljeni u \u010dasopisu Geologica Acta prikazuju prve detaljne mineralo\u0161ke, petrolo\u0161ke, geokemijske i izotopne podatke uklju\u010duju\u0107i i K-Ar starost (gornji anizik-donji […]<\/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-39016","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39016","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=39016"}],"version-history":[{"count":3,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39016\/revisions"}],"predecessor-version":[{"id":39027,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39016\/revisions\/39027"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=39016"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}