{"id":38077,"date":"2021-01-11T09:02:42","date_gmt":"2021-01-11T09:02:42","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=38077"},"modified":"2021-01-11T09:04:29","modified_gmt":"2021-01-11T09:04:29","slug":"sm-nd-geochronology-and-petrologic-investigation-of-sub-ophiolite-metamorphic-sole-from-the-dinarides-krivaja-konjuh-ophiolite-complex-bosnia-and-herzegovina","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/sm-nd-geochronology-and-petrologic-investigation-of-sub-ophiolite-metamorphic-sole-from-the-dinarides-krivaja-konjuh-ophiolite-complex-bosnia-and-herzegovina\/","title":{"rendered":"Sm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina)"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; fullwidth=&#8221;on&#8221; _builder_version=&#8221;4.4.1&#8243; custom_padding=&#8221;0px||0px|||&#8221;][et_pb_fullwidth_slider _builder_version=&#8221;4.4.2&#8243; 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sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#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; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#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; 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;4.4.2&#8243;][et_pb_row _builder_version=&#8221;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.6.6&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243;]<\/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;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.7.7&#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; sticky_enabled=&#8221;0&#8243;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\">Sm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina)<\/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;4.4.2&#8243; custom_padding=&#8221;20px||41px|||&#8221;][et_pb_row _builder_version=&#8221;4.4.2&#8243; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_image src=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/croatica_logo.jpg&#8221; title_text=&#8221;croatica_logo&#8221; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.7.7&#8243; width=&#8221;35%&#8221; max_width=&#8221;30%&#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; alt=&#8221;Geologia Croatica logo&#8221; sticky_enabled=&#8221;0&#8243;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.0.3&#8243; min_height=&#8221;192px&#8221; custom_margin=&#8221;12px|auto||auto||&#8221; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.0.3&#8243;][et_pb_text _builder_version=&#8221;4.7.7&#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; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p>Rezultati istra\u017eivanja me\u0111unarodnog tima znanstvenika s Texas Tech University, Lubbock, USA (Branimir \u0160egvi\u0107, Luka Badurina), HGI-a (Damir Slovenec), Geological Survey of Austria, Vienna, Austria (Ralf Schuster), Sveu\u010dili\u0161ta iz Tuzle, Bosna i Hercegovina (Elvir Babaji\u0107) i Sveu\u010dili\u0161ta iz Zagreba (Bo\u0161ko Lugovi\u0107) rezultirali su objavljivanjem znanstvenog rada naslova \u201eSm-Nd geochronology and petrologic investigationof a sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh Ophiolite Complex, Bosnia and Herzegovina) u \u010dasopisu Geologia Croatica\u201c.<\/p>\n<p>Istra\u017eivanja Krivaja-Konjuh ofiolitnog kompleksa u Bosni i Hrecegovini ukazuju da je Dinaridski segment Neotetisa tijekom srednje jure bio zahva\u0107en \u0161iroko rasprostranjenom konzumacijom oceanske kore i s time povezanim subdukcijsko-akrecijsko-obdukcijskim procesima. Istra\u017eena metamorfna podloga zastupljena amfibolitima granulitnog facijesa, koja je klju\u010dna za razumijevanje dinamike inicijacije intraoceanske subdukcije, na temelju Sm-Nd geokronologije (\u2248 162-160 \u00b1 6-7 Ma) indicira najgornju srednjojursku strarost metamorfizma. Fazni teksturni odnosi ukazuju na vr\u0161ni tlak ravnote\u017ee metamorfizma i temperaturu od ~ 1 GPa, odnosno ~ 800 \u00b0 C. Indiciran je multifazni metamorfizam magmatskog protolita koji je doveo do rekristalizacije primarnog klinopiroksena i plagioklasa, epitaksijskog rasta amfibola i blastoze granata. Dinaridski segment Neotetisa brzo se razvio (unutar ~ 25 Ma) iz aktivnog grebena koji se \u0161irio kroz fazu intraoceanske subdukcije i lu\u010dnog magmatizma do ekshumacije sub-ofiolita i daljnje obdukcije du\u017e pasivnog ruba Adrije na kraju jurske ere.<\/p>\n<p>Rad je dostupan na poveznici: <a href=\"http:\/\/www.geologia-croatica.hr\/index.php\/GC\/article\/view\/996\"><em><a>http:\/\/www.geologia-croatica.hr\/index.php\/GC\/article\/view\/996<\/a> .\u00a0<\/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 RADOVISm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina) Rezultati istra\u017eivanja me\u0111unarodnog tima znanstvenika s Texas Tech University, Lubbock, USA (Branimir \u0160egvi\u0107, Luka Badurina), HGI-a (Damir Slovenec), Geological Survey of Austria, Vienna, Austria (Ralf Schuster), Sveu\u010dili\u0161ta iz Tuzle, Bosna i Hercegovina (Elvir Babaji\u0107) i [&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-38077","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\/sm-nd-geochronology-and-petrologic-investigation-of-sub-ophiolite-metamorphic-sole-from-the-dinarides-krivaja-konjuh-ophiolite-complex-bosnia-and-herzegovina\/\" \/>\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 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