{"id":40826,"date":"2022-03-30T07:43:19","date_gmt":"2022-03-30T07:43:19","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=40826"},"modified":"2023-10-17T10:11:35","modified_gmt":"2023-10-17T10:11:35","slug":"najnoviji-objavljeni-radovi-3","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/najnoviji-objavljeni-radovi-3\/","title":{"rendered":"Najnoviji objavljeni radovi 3"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}”][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=”{}”][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”][\/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”][\/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”][\/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”][\/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”][\/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”][\/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”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”20px||41px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ custom_margin=”|auto|35px|auto||” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_text _builder_version=”4.16″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}”]<\/p>\n

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

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_5,1_5,1_5,1_5,1_5″ use_custom_gutter=”on” gutter_width=”2″ make_equal=”on” padding_top_bottom_link_2=”true” padding_left_right_link_2=”true” _builder_version=”4.16″ custom_margin=”35px|auto||auto||” custom_padding=”2px|0px|6px|0px|false|true” global_colors_info=”{}”][et_pb_column type=”1_5″ _builder_version=”4.16″ background_color=”#ffffff” background_enable_image=”off” custom_padding=”0px||0px||false|false” border_radii=”off|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.16″ header_font=”||||||||” header_3_font=”|800|||||||” header_3_text_color=”#f7f7f7″ header_3_font_size=”25px” header_3_line_height=”1.2em” header_5_text_color=”#1e5096″ header_5_line_height=”1.2em” custom_margin=”20px||6px||false|false” custom_padding=”||0px|20px|false|false” animation_direction=”left” header_3_text_shadow_style=”preset2″ header_3_text_shadow_color=”rgba(0,0,0,0.6)” header_5_text_shadow_style=”preset1″ global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Correlation of upper Miocene-Pliocene Lake Pannon deposits across the Drava Basin, Croatia and Hungary<\/h5>\n

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Paleoecological and sedimentological characterisation of Middle Miocene sediments from the Hrvatska Kostajnica area (Croatia)<\/h5>\n

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<\/strong>Sm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina)<\/h5>\n

[\/et_pb_text][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” _builder_version=”4.16″ _module_preset=”default” custom_margin=”30px||||false|false” custom_padding=”0px||||false|false” global_colors_info=”{}” theme_builder_area=”post_content”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/sm-nd-geochronology-and-petrologic-investigation-of-sub-ophiolite-metamorphic-sole-from-the-dinarides-krivaja-konjuh-ophiolite-complex-bosnia-and-herzegovina\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.16″ custom_button=”on” button_text_size=”16px” button_text_color=”#FFFFFF” button_bg_color=”#d38c3f” button_border_width=”0px” button_border_radius=”10px” button_font=”|||on|||||” button_use_icon=”off” custom_margin=”61px|20px|20px|20px|false|false” custom_padding=”|25px|4px|25px|false|true” global_colors_info=”{}” theme_builder_area=”post_content”][\/et_pb_button][\/et_pb_column][et_pb_column type=”1_5″ _builder_version=”4.16″ background_color=”#ffffff” background_enable_image=”off” custom_padding=”0px||0px||false|false” border_radii=”off|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.16″ header_font=”||||||||” header_3_font=”|800|||||||” header_3_text_color=”#f7f7f7″ header_3_font_size=”25px” header_3_line_height=”1.2em” header_5_text_color=”#1e5096″ header_5_line_height=”1.2em” custom_margin=”20px||6px||false|false” custom_padding=”||0px|20px|false|false” animation_direction=”left” link_option_url=”https:\/\/www.hgi-cgs.hr\/an-ensialic-volcanic-arc-along-the-northwestern-edge-of-palaeotethys-insights-from-the-mid%e2%80%90triassic-volcano%e2%80%90sedimentary-succession-of-ivanscica-mt-northwestern-croatia\/” header_3_text_shadow_style=”preset2″ header_3_text_shadow_color=”rgba(0,0,0,0.6)” header_5_text_shadow_style=”preset1″ global_colors_info=”{}”]<\/p>\n

An ensialic volcanic arc along the northwestern edge of Palaeotethys\u2014Insights from the Mid\u2010Triassic volcano\u2010sedimentary succession of Ivan\u0161\u010dica Mt. (northwestern Croatia<\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2021\/01\/2.-Geological-Journal_logo-1.jpg” alt=”water journal logo” title_text=”2. Geological Journal_logo” _builder_version=”4.16″ _module_preset=”default” custom_margin=”50px|||||” custom_padding=”0px||15px||false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/an-ensialic-volcanic-arc-along-the-northwestern-edge-of-palaeotethys-insights-from-the-mid%e2%80%90triassic-volcano%e2%80%90sedimentary-succession-of-ivanscica-mt-northwestern-croatia\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.16″ custom_button=”on” button_text_size=”16px” button_text_color=”#FFFFFF” button_bg_color=”#d38c3f” button_border_width=”0px” button_border_radius=”10px” button_font=”|||on|||||” button_use_icon=”off” custom_margin=”88px|20px|0px|20px|false|false” custom_padding=”|25px|4px|25px|false|true” global_colors_info=”{}”][\/et_pb_button][\/et_pb_column][et_pb_column type=”1_5″ _builder_version=”4.16″ background_color=”#ffffff” background_enable_image=”off” custom_padding=”0px||0px||false|false” border_radii=”off|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.16″ header_font=”||||||||” header_3_font=”|800|||||||” header_3_text_color=”#f7f7f7″ header_3_font_size=”25px” header_3_line_height=”1.2em” header_5_text_color=”#1e5096″ header_5_line_height=”1.2em” custom_margin=”20px||6px||false|false” custom_padding=”||0px|20px|false|false” animation_direction=”left” link_option_url=”https:\/\/www.hgi-cgs.hr\/the-early-paleozoic-cumulate-gabbroic-rocks-from-the-southwest-part-of-the-tisza-mega-unit-mt-papuk-ne-croatia-evidence-of-a-gondwana-suture-zone\/” header_3_text_shadow_style=”preset2″ header_3_text_shadow_color=”rgba(0,0,0,0.6)” header_5_text_shadow_style=”preset1″ global_colors_info=”{}”]<\/p>\n

The early Paleozoic cumulate gabbroic rocks from the southwest part of the Tisza Mega-Unit (Mt. Papuk, NE Croatia): evidence of a Gondwana suture zone<\/h5>\n

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New dasycladalean alga with unusual two types of laterals from the Palaocene deposits of Konavle, SE of Dubrovnik (Dinarides, Croatia)<\/strong><\/h5>\n

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Regional Isotopic Signatures of Groundwater in Croatia<\/h5>\n

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Petra Bajo objavila je rad u presti\u017enom \u010dasopisu Science:
Persistent influence of obliquity on ice-age terminations since the Middle Pleistocene transition<\/h5>\n

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Objavljen prvi znanstveni rad o zagreba\u010dkom potresu<\/h5>\n

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Ostracods and the middle Miocene evolution of the Bugojno Basin (Bosnia and Herzegovina)<\/h5>\n

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Envekadea vranaensis<\/i> sp. nov. a new diatom species (Bacillariophyta) from the lacustrine Holocene sediments of Lake Vrana, Croatia<\/h5>\n

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Climate Change Impacts on Groundwater Resources in the Coastal Karstic Adriatic Area: A Case Study from the Dinaric Karst<\/h5>\n

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1<\/a>\u00a0\u00a02<\/a>\u00a0 3<\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVICorrelation of upper Miocene-Pliocene Lake Pannon deposits across the Drava Basin, Croatia and HungaryPaleoecological and sedimentological characterisation of Middle Miocene sediments from the Hrvatska Kostajnica area (Croatia)Sm-Nd geochronology and petrologic investigation of sub-ophiolite metamorphic sole from the Dinarides (Krivaja-Konjuh, Ophiolite Complex, Bosnia and Herzegovina)An ensialic volcanic arc along the northwestern edge of Palaeotethys\u2014Insights […]<\/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-40826","page","type-page","status-publish","hentry"],"aioseo_notices":[],"aioseo_head":"\n\t\t\n\t\n\t\n\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t\n\t\t