{"id":39902,"date":"2021-08-16T08:00:20","date_gmt":"2021-08-16T08:00:20","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=39902"},"modified":"2021-08-16T08:02:57","modified_gmt":"2021-08-16T08:02:57","slug":"karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/","title":{"rendered":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives"},"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; min_height=&#8221;112px&#8221; height=&#8221;400px&#8221; custom_margin=&#8221;0px||||false|false&#8221; custom_padding=&#8221;0px||18px||false|false&#8221; auto=&#8221;on&#8221; auto_ignore_hover=&#8221;on&#8221; locked=&#8221;off&#8221;][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\/Br\u010di\u0107_Drvenik02-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\/ban2-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\/20190228_094232-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\/ban3-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\/Bijele_stijene-Gorski_kotar-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\/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;4.9.10&#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;\">Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives<\/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;4.7.4&#8243; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.7.4&#8243;][et_pb_image src=&#8221;https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2021\/08\/ijes1.jpg&#8221; alt=&#8221;Frontiers naslovnica&#8221; title_text=&#8221;ijes1&#8243; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.9.10&#8243; width=&#8221;100%&#8221; max_width=&#8221;85%&#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; 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;4.9.10&#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>U znanstvenom \u010dasopisu <em>International Journal of Earth Sciences<\/em> objavljen je znanstveni rad pod naslovom <em>Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives<\/em>. Rad je rezultat suradnje znanstvenika iz Hrvatskog geolo\u0161kog instituta, Sveu\u010dili\u0161ta u \u017denevi, Sveu\u010dili\u0161ta Basilicata, Sveu\u010dili\u0161ta u Zaragozi, Geolo\u0161kog instituta Bugarske Akademije Znanosti, Britanskog geolo\u0161kog instituta te INA-Industrija nafte d.d..<\/p>\n<p>U radu su multidisciplinarnim pristupom istra\u017eivani kr\u0161ki boksiti le\u017ei\u0161ta Crveni Klanac (okolica Trilja, sredi\u0161nja Dalmacija) razvijeni u gornjokrednim platformnim vapnencima, koji se nalaze u podini miocenskih jezerskih naslaga Sinjskog bazena (dio Dinaridskog jezerskog sustava). Na autohtonost boksita upu\u0107uje <em>in situ<\/em> mineralizacija dominantno predstavljena autigenim kaolinitom i gibsitom. Razli\u010diti stratigrafski horizonti boksitnog profila karakterizirani su sli\u010dnim oligocenskim i miocenskim <em>in situ<\/em> U-Pb starostima cirkona, \u0161to upu\u0107uje na isto izvori\u0161te materijala za boksitizaciju. Maksimalna starost talo\u017eenja izvori\u0161nog materijala iz kojeg su boksiti nastali, koja ujedno predstavlja i maksimalnu starost autohtone boksitizacije, dobivena je putem vrlo preciznog CA-ID-TIMS U-Pb datiranja cirkona te iznosi 16.9576 \u00b1 0.021 milijuna godina. Navedena starost koincidira s po\u010detkom miocenskog klimatskog optimuma \u2013 razdoblja globalnog zatopljenja tijekom kenozoika koje je trajalo od 17 do 14.7 milijuna godina. Da bi se autohtona boksitizacija, koja je prema dostupnim geokronolo\u0161kim podacima trajala manje od 700 000 godina, mogla odvijati na jugoisto\u010dnom dijelu kontinentalne Europe tijekom miocenskog klimatskog optimuma, srednje godi\u0161nje vrijednosti temperature zraka morale su biti vi\u0161e od 17\u201322 \u00b0C, a srednje godi\u0161nje koli\u010dine oborina ve\u0107e od 1100<span>\u2013<\/span>1200 mm.<\/p>\n<p>Dobiveni novi podaci predstavljaju temelj i smjernice za daljnje utvr\u0111ivanje uloge kenozojskih kr\u0161kih boksita Dinarida kao zapisa geneze boksita, provenijencije te paleoklimatologije.<\/p>\n<p>Istra\u017eivanje je napravljeno 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).<\/p>\n<p>Rad je dostupan na sljede\u0107oj poveznici:\u00a0<a href=\"https:\/\/link.springer.com\/article\/10.1007\/s00531-021-02091-z\"><em>https:\/\/link.springer.com\/article\/10.1007\/s00531-021-02091-z<\/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 RADOVIKarst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectivesU znanstvenom \u010dasopisu International Journal of Earth Sciences objavljen je znanstveni rad pod naslovom Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives. Rad je rezultat suradnje znanstvenika iz Hrvatskog geolo\u0161kog instituta, Sveu\u010dili\u0161ta [&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-39902","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\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/\" \/>\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 geolo\u0161ki institut |\" \/>\n\t\t<meta property=\"og:type\" content=\"article\" \/>\n\t\t<meta property=\"og:title\" content=\"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\u0161ki institut\" \/>\n\t\t<meta property=\"og:url\" content=\"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/\" \/>\n\t\t<meta property=\"article:published_time\" content=\"2021-08-16T08:00:20+00:00\" \/>\n\t\t<meta property=\"article:modified_time\" content=\"2021-08-16T08:02:57+00:00\" \/>\n\t\t<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/HGI.CGS\/\" \/>\n\t\t<meta name=\"twitter:card\" content=\"summary\" \/>\n\t\t<meta name=\"twitter:title\" content=\"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\u0161ki institut\" \/>\n\t\t<script type=\"application\/ld+json\" class=\"aioseo-schema\">\n\t\t\t{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#breadcrumblist\",\"itemListElement\":[{\"@type\":\"ListItem\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en#listItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\",\"nextItem\":{\"@type\":\"ListItem\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#listItem\",\"name\":\"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives\"}},{\"@type\":\"ListItem\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#listItem\",\"position\":2,\"name\":\"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives\",\"previousItem\":{\"@type\":\"ListItem\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en#listItem\",\"name\":\"Home\"}}]},{\"@type\":\"Organization\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/#organization\",\"name\":\"Hrvatski geolo\\u0161ki institut\",\"description\":\"Hrvatski geolo\\u0161ki institut najve\\u0107i je istra\\u017eiva\\u010dki institut u podru\\u010dju geoznanosti i geolo\\u0161kog in\\u017eenjerstva u Republici Hrvatskoj.\",\"url\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/\",\"email\":\"ibutorac@hgi-cgs.hr\",\"telephone\":\"+38516160888\",\"logo\":{\"@type\":\"ImageObject\",\"url\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/wp-content\\\/uploads\\\/2026\\\/04\\\/hgi-sluzbeni-logo.jpg\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#organizationLogo\",\"width\":96,\"height\":45},\"image\":{\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#organizationLogo\"},\"sameAs\":[\"https:\\\/\\\/www.facebook.com\\\/HGI.CGS\\\/\"]},{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#webpage\",\"url\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/\",\"name\":\"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\\u0161ki institut\",\"inLanguage\":\"en-US\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/#website\"},\"breadcrumb\":{\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\\\/#breadcrumblist\"},\"datePublished\":\"2021-08-16T08:00:20+00:00\",\"dateModified\":\"2021-08-16T08:02:57+00:00\"},{\"@type\":\"WebSite\",\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/#website\",\"url\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/\",\"name\":\"Hrvatski geolo\\u0161ki institut\",\"inLanguage\":\"en-US\",\"publisher\":{\"@id\":\"https:\\\/\\\/www.hgi-cgs.hr\\\/en\\\/#organization\"}}]}\n\t\t<\/script>\n\t\t<!-- All in One SEO -->\n\n","aioseo_head_json":{"title":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\u0161ki institut","description":"","canonical_url":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/","robots":"max-image-preview:large","keywords":"","webmasterTools":{"miscellaneous":""},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"BreadcrumbList","@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#breadcrumblist","itemListElement":[{"@type":"ListItem","@id":"https:\/\/www.hgi-cgs.hr\/en#listItem","position":1,"name":"Home","item":"https:\/\/www.hgi-cgs.hr\/en","nextItem":{"@type":"ListItem","@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#listItem","name":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives"}},{"@type":"ListItem","@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#listItem","position":2,"name":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives","previousItem":{"@type":"ListItem","@id":"https:\/\/www.hgi-cgs.hr\/en#listItem","name":"Home"}}]},{"@type":"Organization","@id":"https:\/\/www.hgi-cgs.hr\/en\/#organization","name":"Hrvatski geolo\u0161ki institut","description":"Hrvatski geolo\u0161ki institut najve\u0107i je istra\u017eiva\u010dki institut u podru\u010dju geoznanosti i geolo\u0161kog in\u017eenjerstva u Republici Hrvatskoj.","url":"https:\/\/www.hgi-cgs.hr\/en\/","email":"ibutorac@hgi-cgs.hr","telephone":"+38516160888","logo":{"@type":"ImageObject","url":"https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2026\/04\/hgi-sluzbeni-logo.jpg","@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#organizationLogo","width":96,"height":45},"image":{"@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#organizationLogo"},"sameAs":["https:\/\/www.facebook.com\/HGI.CGS\/"]},{"@type":"WebPage","@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#webpage","url":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/","name":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\u0161ki institut","inLanguage":"en-US","isPartOf":{"@id":"https:\/\/www.hgi-cgs.hr\/en\/#website"},"breadcrumb":{"@id":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/#breadcrumblist"},"datePublished":"2021-08-16T08:00:20+00:00","dateModified":"2021-08-16T08:02:57+00:00"},{"@type":"WebSite","@id":"https:\/\/www.hgi-cgs.hr\/en\/#website","url":"https:\/\/www.hgi-cgs.hr\/en\/","name":"Hrvatski geolo\u0161ki institut","inLanguage":"en-US","publisher":{"@id":"https:\/\/www.hgi-cgs.hr\/en\/#organization"}}]},"og:locale":"en_US","og:site_name":"Hrvatski geolo\u0161ki institut |","og:type":"article","og:title":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\u0161ki institut","og:url":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/","article:published_time":"2021-08-16T08:00:20+00:00","article:modified_time":"2021-08-16T08:02:57+00:00","article:publisher":"https:\/\/www.facebook.com\/HGI.CGS\/","twitter:card":"summary","twitter:title":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives | Hrvatski geolo\u0161ki institut"},"aioseo_meta_data":{"post_id":"39902","title":null,"description":null,"keywords":[],"keyphrases":{"focus":[],"additional":[]},"primary_term":null,"canonical_url":null,"og_title":null,"og_description":null,"og_object_type":"default","og_image_type":"default","og_image_url":null,"og_image_width":null,"og_image_height":null,"og_image_custom_url":null,"og_image_custom_fields":null,"og_video":"","og_custom_url":null,"og_article_section":null,"og_article_tags":[],"twitter_use_og":false,"twitter_card":"default","twitter_image_type":"default","twitter_image_url":null,"twitter_image_custom_url":null,"twitter_image_custom_fields":null,"twitter_title":null,"twitter_description":null,"schema":{"blockGraphs":[],"customGraphs":[],"default":{"data":{"Article":[],"Course":[],"Dataset":[],"FAQPage":[],"Movie":[],"Person":[],"Product":[],"ProductReview":[],"Car":[],"Recipe":[],"Service":[],"SoftwareApplication":[],"WebPage":[]},"graphName":"","isEnabled":true},"graphs":[],"defaultGraph":"WebPage","defaultPostTypeGraph":""},"schema_type":"default","schema_type_options":"{\"article\":{\"articleType\":\"BlogPosting\"},\"course\":{\"name\":\"\",\"description\":\"\",\"provider\":\"\"},\"faq\":{\"pages\":[]},\"product\":{\"reviews\":[]},\"recipe\":{\"ingredients\":[],\"instructions\":[],\"keywords\":[]},\"software\":{\"reviews\":[],\"operatingSystems\":[]},\"webPage\":{\"webPageType\":\"WebPage\"}}","pillar_content":false,"robots_default":true,"robots_noindex":false,"robots_noarchive":false,"robots_nosnippet":false,"robots_nofollow":false,"robots_noimageindex":false,"robots_noodp":false,"robots_notranslate":false,"robots_max_snippet":"-1","robots_max_videopreview":"-1","robots_max_imagepreview":"large","priority":null,"frequency":"default","local_seo":{"locations":{"business":{"name":"","businessType":"","image":"","areaServed":"","urls":{"website":"","aboutPage":"","contactPage":""},"address":{"streetLine1":"","streetLine2":"","zipCode":"","city":"","state":"","country":"","addressFormat":"#streetLineOne\n#streetLineTwo\n#city, #state #zipCode"},"contact":{"email":"","phone":"","phoneFormatted":"","fax":"","faxFormatted":""},"ids":{"vat":"","tax":"","chamberOfCommerce":""},"payment":{"priceRange":"","currenciesAccepted":"","methods":""}}},"openingHours":{"useDefaults":true,"show":true,"alwaysOpen":false,"use24hFormat":false,"timezone":"","labels":{"closed":"","alwaysOpen":""},"days":{"monday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"},"tuesday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"},"wednesday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"},"thursday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"},"friday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"},"saturday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"},"sunday":{"open24h":false,"closed":false,"openTime":"09:00","closeTime":"17:00"}}}},"breadcrumb_settings":null,"limit_modified_date":false,"ai":null,"created":"2021-08-16 08:00:06","updated":"2025-06-09 15:26:38","seo_analyzer_scan_date":null},"aioseo_breadcrumb":"<div class=\"aioseo-breadcrumbs\"><span class=\"aioseo-breadcrumb\">\n\t\t\t<a href=\"https:\/\/www.hgi-cgs.hr\/en\" title=\"Home\">Home<\/a>\n\t\t<\/span><span class=\"aioseo-breadcrumb-separator\">&raquo;<\/span><span class=\"aioseo-breadcrumb\">\n\t\t\tKarst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives\n\t\t<\/span><\/div>","aioseo_breadcrumb_json":[{"label":"Home","link":"https:\/\/www.hgi-cgs.hr\/en"},{"label":"Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives","link":"https:\/\/www.hgi-cgs.hr\/en\/karst-bauxite-formation-during-miocene-climatic-optimum-central-dalmatia-croatia-mineralogical-compositional-and-geochronological-perspectives\/"}],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39902","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=39902"}],"version-history":[{"count":2,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39902\/revisions"}],"predecessor-version":[{"id":39906,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39902\/revisions\/39906"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=39902"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}