{"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":"

[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

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Sm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina)<\/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\/2020\/11\/croatica_logo.jpg” title_text=”croatica_logo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.7.7″ width=”35%” max_width=”30%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” alt=”Geologia Croatica logo” sticky_enabled=”0″][\/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=”4.7.7″ 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 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

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

Rad je dostupan na poveznici: http:\/\/www.geologia-croatica.hr\/index.php\/GC\/article\/view\/996<\/a> .\u00a0<\/em><\/a><\/p>\n

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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 […]<\/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":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/38077","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=38077"}],"version-history":[{"count":3,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/38077\/revisions"}],"predecessor-version":[{"id":38081,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/38077\/revisions\/38081"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=38077"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}