{"id":39649,"date":"2021-06-24T07:48:30","date_gmt":"2021-06-24T07:48:30","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=39649"},"modified":"2023-10-17T10:20:07","modified_gmt":"2023-10-17T10:20:07","slug":"najnoviji-objavljeni-radovi-2","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/najnoviji-objavljeni-radovi-2\/","title":{"rendered":"Najnoviji objavljeni radovi 2"},"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|0px|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

Middle Triassic lake deepening in the Ordos Basin of North China linked with global sea-level rise<\/span><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2021\/10\/X09218181-1.jpg” alt=”Global and Planetary Change” title_text=”X09218181-1″ _builder_version=”4.16″ _module_preset=”default” width=”100%” custom_margin=”85px||||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}” theme_builder_area=”post_content”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/middle-triassic-lake-deepening-in-the-ordos-basin-of-north-china-linked-with-global-sea-level-rise\/” 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=”105px|20px|20px|20px|false|false” custom_padding=”|25px|4px|25px||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” 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

Numerical modeling as a tool for evaluating the renewability of geothermal resources: the case study of the Euganean Geothermal System (NE Italy)<\/h5>\n

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Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives\u00a0<\/h5>\n

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Geometric and Fractal Characterization of Pore Systems in the Upper Triassic Dolomites Based on Image Processing Techniques (Example from \u017dumberak Mts, NW Croatia)<\/h5>\n

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Miocene tuffs from the Dinarides and Eastern Alps as proxies of the Pannonian Basin lithosphere dynamics and tropospheric circulation patterns in Central Europe<\/strong><\/h5>\n

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Changes in Cave Sedimentation Mechanisms During the Late Quaternary: An Example From the Lower Cerova\u010dka Cave, Croatia<\/strong><\/h5>\n

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Comparison of measured and estimated permeability for artificially prepared coarse-grained soil samples<\/h5>\n

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Past climate variations recorded in needle-like aragonites correlate with organic carbon burial efficiency as revealed by lake sediments in Croatia<\/h5>\n

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Cenomanian\u2013Turonian Oceanic Anoxic Event (OAE2) imprint on the northwestern part of the Adriatic Carbonate Platform and a coeval intra-platform basin (Istria and Premuda Island, Croatia)<\/span><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2021\/04\/cre.jpg” alt=”water journal logo” title_text=”cre” _builder_version=”4.16″ _module_preset=”default” width=”100%” custom_margin=”8px||||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/cenomanian-turonian-oceanic-anoxic-event-oae2-imprint-on-the-northwestern-part-of-the-adriatic-carbonate-platform-and-a-coeval-intra-platform-basin-istria-and-premuda-island-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=”115px|20px|11px|20px|false|false” custom_padding=”|25px|4px|25px||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” 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

Impact of Land Use on Karst Water Resources\u2014A Case Study of the Kupa (Kolpa) Transboundary River Catchment\u00a0<\/h5>\n

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Structural setting and geodynamics of the Kvarner area (Northern Adriatic)<\/h5>\n

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Regional-Scale Landslide Susceptibility Mapping Using Limited LiDAR-Based Landslide Inventories for Sisak-Moslavina County, Croatia<\/h5>\n

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Middle Triassic high-K calc-alkaline effusive and pyroclastic rocks from the Zagorje-Mid-Transdanubian Zone (Mt. Kuna Gora; NW Croatia): mineralogy, petrology, geochemistry and tectonomagmatic affinity<\/h5>\n

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Destructive M6.2 Petrinja Earthquake (Croatia) in 2020\u2014Preliminary Multidisciplinary Research<\/h5>\n

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Tidal deposits in the Early Miocene Central Paratethys: the Vu\u010dji Jarek and \u010cemernica members of the Macelj formation (NW Croatia)<\/h5>\n

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Active tectonics in the Kvarner region (External Dinarides, Croatia) \u2013 an alternative approach based on focused geological mapping, 3D seismological and shallow seismic imaging data<\/span><\/h5>\n

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Paleoenvironmental changes and vegetation of the Transylvanian Basin in the early stages of Lake Pannon (late Miocene, Tortonian)<\/strong><\/h5>\n

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Salt pans as a new archaeological sea-level proxy: A test case from Dalmatia, Croatia<\/span><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/qscience.png” alt=”Geosciences logo” title_text=”qscience” _builder_version=”4.16″ _module_preset=”default” custom_margin=”70px||||false|false” custom_padding=”12px||||false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/salt-pans-as-a-new-archaeological-sea-level-proxy-a-test-case-from-dalmatia-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=”75px|20px|20px|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” 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

Sarmatian biostratigraphy of a marginal sea in northern Croatia based on calcareous nannofossils<\/span><\/h5>\n

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Geomorphology of Canyon Outlets in Zrmanja River Estuary and Its Effect on the Holocene Flooding of Semi-enclosed Basins (the Novigrad and Karin Seas, Eastern Adriatic)<\/h5>\n

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

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NAJNOVIJI OBJAVLJENI RADOVIMiddle Triassic lake deepening in the Ordos Basin of North China linked with global sea-level riseNumerical modeling as a tool for evaluating the renewability of geothermal resources: the case study of the Euganean Geothermal System (NE Italy)Karst bauxite formation during Miocene Climatic Optimum (central Dalmatia, Croatia): mineralogical, compositional and geochronological perspectives\u00a0Geometric and Fractal […]<\/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-39649","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39649","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=39649"}],"version-history":[{"count":34,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39649\/revisions"}],"predecessor-version":[{"id":42603,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/39649\/revisions\/42603"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=39649"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}