{"id":43754,"date":"2024-06-03T06:57:29","date_gmt":"2024-06-03T06:57:29","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=43754"},"modified":"2024-06-03T06:59:43","modified_gmt":"2024-06-03T06:59:43","slug":"middle-triassic-basaltic-pyroclastic-rocks-from-the-mt-medvednica-ophiolite-melange-nw-croatia-petrology-geochemistry-and-tectono-magmatic-setting","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/middle-triassic-basaltic-pyroclastic-rocks-from-the-mt-medvednica-ophiolite-melange-nw-croatia-petrology-geochemistry-and-tectono-magmatic-setting\/","title":{"rendered":"Middle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolite m\u00e9lange (NW Croatia): petrology, geochemistry and tectono-magmatic setting"},"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=”4.25.1″ 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

Middle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolite m\u00e9lange (NW Croatia): petrology, geochemistry and tectono-magmatic setting<\/strong><\/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\/2020\/11\/croatica_logo.jpg” alt=”Geologia Croatica logo” title_text=”croatica_logo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.25.1″ width=”25%” max_width=”49%” 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=”4.25.1″ 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

Rezultati istra\u017eivanja projekta GOST (IP-2019-04-3824) Hrvatske zaklade za znanost objavljeni u \u010dasopisu Geologia Croatica daju prve detaljne geolo\u0161ke, mineralo\u0161ke, petrolo\u0161ke i geokemijske podatke o hektometarskim blokovima srednjotrijaskih mafitnih piroklasti\u010dnih stijena (vulkanskih aglomerata\/bre\u010da i lapilnih tufova) inkorporiranih u ofiolitnom melan\u017eu Medvednice, smje\u0161tenom u jugozapadnom segmentu Zagorje-Srednje-Transdanubijske zone. Ove stijene dijele petrokemijske karakteristike s piroklasti\u010dnim derivatima alkalijskih bazaltnih lava nastalim unutar plo\u010de, danas arhiviranim u ofiolitnim melan\u017eima Samoborske gore i Kalnika. Formiranje ovih pre-ofiolitskih piroklasti\u010dnih stijena povezano je s intrakontinentalnim riftnim procesima i odra\u017eava taljevine nastale iz oboga\u0107enog pla\u0161tnog izvori\u0161ta OIB tipa. Formiranje istra\u017eivanih piroklastita zbivalo se tijekom kasnog anizika-ranog ladinika du\u017e kontinentalnog ruba Palaeotetisa kroz proto zlau\u010dni rifting kontinentalne litosfere (Adria plo\u010da) \u0161to je dovelo do formiranja Maliak\/Balkanskog rifta u nastaju\u0107em sjeverozapadnom segmentu Neotetisa.<\/p>\n

\u00a0Rad je dostupan na poveznici: http:\/\/www.geologia-croatica.hr\/index.php\/GC\/issue\/view\/86<\/em><\/a><\/p>\n

 <\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVIMiddle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolite m\u00e9lange (NW Croatia): petrology, geochemistry and tectono-magmatic settingRezultati istra\u017eivanja projekta GOST (IP-2019-04-3824) Hrvatske zaklade za znanost objavljeni u \u010dasopisu Geologia Croatica daju prve detaljne geolo\u0161ke, mineralo\u0161ke, petrolo\u0161ke i geokemijske podatke o hektometarskim blokovima srednjotrijaskih mafitnih piroklasti\u010dnih stijena (vulkanskih aglomerata\/bre\u010da i lapilnih tufova) inkorporiranih […]<\/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-43754","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/43754","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=43754"}],"version-history":[{"count":3,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/43754\/revisions"}],"predecessor-version":[{"id":43758,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/43754\/revisions\/43758"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=43754"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}