{"id":36560,"date":"2020-11-11T10:26:29","date_gmt":"2020-11-11T10:26:29","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=36560"},"modified":"2025-06-20T06:18:53","modified_gmt":"2025-06-20T06:18:53","slug":"najnoviji-objavljeni-radovi","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/najnoviji-objavljeni-radovi\/","title":{"rendered":"Najnoviji objavljeni radovi"},"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=”4.27.4″ custom_margin=”-8px|auto|20px|auto|false|false” custom_padding=”2px|0px|15px|0px|false|true” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][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=”|||” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.4″ 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||29px||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″ locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Late Quaternary geomorphology and sedimentary processes in the Prolo\u0161ko Blato karst wetland (Imotsko Polje, Croatia)<\/h5>\n
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[\/et_pb_text][et_pb_image src=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/05\/geomorf.jpg” alt=”Geologia Croatica logo” title_text=”geomorf” disabled_on=”off|off|off” _builder_version=”4.27.4″ _module_preset=”default” width=”100%” custom_margin=”49px||0px||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\/late-quaternary-geomorphology-and-sedimentary-processes-in-the-prolosko-blato-karst-wetland-imotsko-polje-croatia\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.4″ 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=”157px|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=”|||” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.4″ 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||29px||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″ locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Holocene paleoenvironmental changes recorded in the sediments of the karst Krka River estuary (eastern Adriatic coast, Croatia)<\/span><\/h5>\n
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[\/et_pb_text][et_pb_image src=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/03\/catena.jpg” alt=”Geologia Croatica logo” title_text=”catena” disabled_on=”off|off|off” _builder_version=”4.27.4″ _module_preset=”default” width=”100%” custom_margin=”10px||0px||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\/holocene-paleoenvironmental-changes-recorded-in-the-sediments-of-the-karst-krka-river-estuary-eastern-adriatic-coast-croatia\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.4″ 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=”136px|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″ admin_label=”Column” _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″ global_colors_info=”{}” custom_padding__hover=”|||” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.4″ 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||29px||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″ locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Defining the geological units susceptible to landslides in Pannonian Croatia using energy relief index<\/em>\u00a0<\/span><\/h5>\n
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[\/et_pb_text][et_pb_image src=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/03\/bulletin-of.jpg” alt=”Geologia Croatica logo” title_text=”bulletin of” disabled_on=”off|off|off” _builder_version=”4.27.4″ _module_preset=”default” width=”100%” custom_margin=”75px||0px||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\/defining-the-geological-units-susceptible-to-landslides-in-pannonian-croatia-using-energy-relief-index\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.4″ 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=”187px|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″ global_colors_info=”{}” custom_padding__hover=”|||” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.4″ 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||29px||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″ locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Croatian Critical Mineral Commodity Letters: Magnesium<\/h5>\n
\u00a0<\/strong><\/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” disabled_on=”off|off|off” _builder_version=”4.27.4″ _module_preset=”default” width=”100%” custom_margin=”75px||0px||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\/croatian-critical-mineral-commodity-letters-magnesium\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.4″ 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=”205px|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″ global_colors_info=”{}” custom_padding__hover=”|||” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2024\/04\/LOGO-002.jpg” alt=”springer” title_text=”LOGO (002)” _builder_version=”4.24.2″ _module_preset=”default” width=”100%” custom_margin=”-84px||10px||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}” theme_builder_area=”post_content”][\/et_pb_image][et_pb_text _builder_version=”4.27.4″ 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||29px||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″ locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Geochemical Insights and Mineral Resource Potential of Rare Earth Elements (REE) in the Croatian Karst Bauxites<\/span><\/h5>\n
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[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/02\/mineralas.jpg” alt=”Geologia Croatica logo” title_text=”minerals” _builder_version=”4.27.4″ _module_preset=”default” width=”100%” custom_margin=”18px||10px||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\/geochemical-insights-and-mineral-resource-potential-of-rare-earth-elements-ree-in-the-croatian-karst-bauxites\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.4″ 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=”221px|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_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=”-8px|auto||auto||” custom_padding=”2px|0px|15px|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″ global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.27.4″ 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||29px||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

Seasonal variability and risk evaluation of emerging organic contaminants in European river: Linking in silico<\/em> and in vitro<\/em> approaches to prioritize hazardous EOCs<\/span><\/h5>\n
\u00a0<\/strong><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/01\/es.jpg” alt=”Geosciences logo” title_text=”es” _builder_version=”4.27.4″ _module_preset=”default” width=”100%” custom_margin=”25px||10px||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/seasonal-variability-and-risk-evaluation-of-emerging-organic-contaminants-in-european-river-linking-in-silico-and-in-vitro-approaches-to-prioritize-hazardous-eocs\/?et_fb=1&PageSpeed=off” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.4″ 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=”135px|20px|20px|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″ global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.27.2″ 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||29px||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

Spread and frequency of explosive silicic volcanism of the Carpathian-Pannonian Region during Early Miocene: Clues from the SW Pannonian Basin and the Dinarides.\u00a0<\/strong><\/h5>\n

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Impact of the Jenkyns Event on shallow-marine carbonates and coeval emerged paleoenvironments: the Plitvice Lakes region, Croatia.\u00a0<\/strong><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2024\/10\/paleo.jpg” alt=”Geosciences logo” title_text=”paleo” _builder_version=”4.27.2″ _module_preset=”default” width=”100%” custom_margin=”49px||10px||false|false” custom_padding=”||9px|0px|false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/impact-of-the-jenkyns-event-on-shallow-marine-carbonates-and-coeval-emerged-paleoenvironments-the-plitvice-lakes-region-croatia\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.2″ 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=”167px|20px|20px|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″ global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.27.2″ 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||29px||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

Unravelling the tectonic evolution of the Dinarides\u2014Alps\u2014Pannonian Basin transition zone: insights from structural analysis and low-temperature thermochronology from Ivan\u0161\u010dica Mt., NW Croatia<\/strong><\/h5>\n

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Mobility patterns of rare earth elements in diagenetically altered vitric tuff shaped by illite-smectite<\/h5>\n

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A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the Dinaride Lake System: implications for tephrostratigraphy and emplacement of volcaniclastic deposits<\/strong><\/h5>\n

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Holocene palaeoenvironmental development of Prokljan Lake (Krka River, Croatia): Evolution from a calcareous tufa barrier system to a karst estuary<\/span><\/h5>\n

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Geological Assessment of Faults in Digitally Processed Aerial Images within Karst Area<\/strong><\/h5>\n

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High-resolution seismic record of the Quaternary palaeoenvironments along a Dalmatian-type coast (Lo\u0161inj Channel, Adriatic Sea)<\/strong><\/h5>\n

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Influence of changing water mass circulation on detrital component and carbon burial of Late Pleistocene and Holocene sediments in the eastern-central Mid-Adriatic Deep<\/span><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2024\/07\/marine.jpg” alt=”Geologia Croatica logo” title_text=”marine” _builder_version=”4.27.0″ _module_preset=”default” width=”100%” custom_margin=”18px||10px||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/influence-of-changing-water-mass-circulation-on-detrital-component-and-carbon-burial-of-late-pleistocene-and-holocene-sediments-in-the-eastern-central-mid-adriatic-deep\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.0″ 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=”135px|20px|20px|20px|false|false” custom_padding=”|25px|4px|25px||true” global_colors_info=”{}”][\/et_pb_button][\/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=”4.27.4″ custom_margin=”20px|auto||auto|false|false” custom_padding=”2px|0px|15px|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″ global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.27.0″ 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||29px||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

A distal record of the Middle Miocene silicic eruption of the Carpathian-Pannonian Region stored within the Dinaride Lake System: implications for tephrostratigraphy and emplacement of volcaniclastic deposits<\/strong><\/h5>\n

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Holocene palaeoenvironmental development of Prokljan Lake (Krka River, Croatia): Evolution from a calcareous tufa barrier system to a karst estuary<\/span><\/h5>\n

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Geological Assessment of Faults in Digitally Processed Aerial Images within Karst Area<\/strong><\/h5>\n

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High-resolution seismic record of the Quaternary palaeoenvironments along a Dalmatian-type coast (Lo\u0161inj Channel, Adriatic Sea)<\/strong><\/h5>\n

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Influence of changing water mass circulation on detrital component and carbon burial of Late Pleistocene and Holocene sediments in the eastern-central Mid-Adriatic Deep<\/span><\/h5>\n

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Hydrochemical characterization of a Dinaric karst catchment in relation to emerging organic contaminants<\/strong><\/h5>\n

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Middle Triassic basaltic pyroclastic rocks from the Mt. Medvednica ophiolite m\u00e9lange (NW Croatia): petrology, geochemistry and tectono-magmatic setting<\/strong><\/h5>\n

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Mammal-bearing Pleistocene deposits, Vrani\u0107, southwestern Pannonian Basin System<\/h5>\n

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Vegetation response to climate change during an Early Jurassic hyperthermal event (Jenkyns Event) from Northern China (Ordos Basin)<\/h5>\n

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Facies architecture, geochemistry and petrogenesis of Middle Triassic volcaniclastic deposits of Mt. Ivan\u0161\u010dica (NW Croatia): evidence of bimodal volcanism in the Alpine-Dinaridic transitional zone<\/h5>\n

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Characterizing occurrence of emerging organic contaminants in Dinaric karst catchment of Jadro and \u017drnovnica springs, Croatia<\/h5>\n

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The early history of the Neotethys archived in the ophiolitic m\u00e9lange of northwestern Croatia<\/h5>\n

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The evolution of the Mesozoic lithosphere of northwestern Neotethys: A petrogenetic and geodynamic perspective<\/em><\/strong><\/h5>\n

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Remote Sensing and GIS in Landslide Management: An Example from the Kravarsko Area, Croatia<\/em><\/strong><\/h5>\n

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Evolution of eastern passive margin of Adria recorded in shallow to deep<\/strong>\u2011water successions of the transition zone between the Alps and the Dinarides (Ivan\u0161\u010dica Mt., NW Croatia)<\/strong><\/h5>\n

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Provenance and depositional environment of Middle Miocene silicic volcaniclastic deposits from Mt. Medvednica (North Croatian Basin, Carpathian-Pannonian Region)<\/strong>\u00a0<\/h5>\n

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A time-space window between Eocene karst bauxite genesis and the first molasse deposition in the Dinaric Foreland Basin in the North Dalmatia, Croatia<\/h5>\n

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Assessing the persistence, mobility and toxicity of emerging organic contaminants in Croatian karst springs used for drinking water supply<\/span><\/h5>\n

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Collapse of terrestrial ecosystems linked to heavy metal poisoning during the Toarcian oceanic anoxic event<\/h5>\n

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Integrated Reconstruction of Late Quaternary Geomorphology and Sediment Dynamics of Prokljan Lake and Krka River Estuary, Croatia<\/strong><\/h5>\n

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Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia<\/h5>\n

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Biostratigraphy and facies description of Middle Triassi rift-related volcano-sedimentary successions at the junction of the Southern Alps and the Dinarides<\/h5>\n

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Rapid Remeasure of Dense Civilian Networks as a Game-Changer Tool for Surface Deformation Monitoring: The Case Study of the M<\/i>w<\/i><\/sub> 6.4 2020 Petrinja Earthquake, Croatia<\/h5>\n

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Relation between relief and Badland spatial distribution in the PaleogenePazin Basin, Croatia<\/h5>\n

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ON THE EVOLUTION OF MIDDLE TRIASSIC PASSIVE MARGINS OF THE GREATER ADRIA PLATE: INFERENCES FROM THE STUDY OF CALC-ALKALINE AND SHOSHONITIC TUFFS FROM NW CROATIA<\/h5>\n

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Triassic evolution of the Adriatic-Dinaridic platform\u2019s continental margins\u2014insights from rare dolerite subvolcanic intrusions in External Dinarides, Croatia <\/span><\/h5>\n

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Tracing widespread Early Miocene ignimbrite eruptions and petrogenesis at the onset of the Carpathian-Pannonian Region silicic volcanism<\/h5>\n

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Landslide monitoring techniques in the Geological Surveys of Europe<\/h5>\n
\u00a0<\/strong><\/h5>\n

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Geochemical records in subaerial exposure environments in Croatia using discriminant function analysis of bauxite data<\/strong><\/h5>\n

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Sub-recent microfauna within allogenic sediments at the bottom of a deep cave, Njemica (Biokovo Mt., Croatia)<\/strong><\/h5>\n

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Multi-Level Data Analyses in the Gajevo Landslide Research, Croatia<\/h5>\n
\u00a0<\/strong><\/h5>\n

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Major and rare earth element mineral chemistry of low-grade assemblages inform dynamics of hydrothermal ocean-floor metamorphism in the Dinaridic Neotethys<\/h5>\n

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Discrimination of Rock Units in Karst Terrains Using Sentinel-2A Imagery<\/h5>\n

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Olujna naslaga krupnoklasti\u010dnog sedimenta i usamljeni olujni blokovi na otoku Mana (NP Kornati) <\/strong><\/h5>\n

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Low-grade metamorphic rocks of the Tethys subduction\u2013collision zone in the Medvednica Mt. (NW Croatia)<\/h5>\n

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Taxonomy of the fossil calcareous algae: Revision of genera Physoporella <\/em>STEINMANN and Oligoporella <\/em>PIA (Dasycladales)<\/h5>\n

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The Impact of Climate Changes on Slope Stability and Landslide Conditioning Factors: An Example from Kravarsko, Croatia<\/h5>\n

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A case study in the research polygon in Glina and Dvor municipality, Croatia\u2013landslide susceptibility assessment of geological units<\/h5>\n

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Preliminary analysis of a LiDAR-based landslide inventory in the area of Samobor, Croatia<\/h5>\n

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Use of a LiDAR-derived landslide inventory map in assessing Influencing factors for landslide susceptibility of geological units in the Petrinja area (Croatia)<\/h5>\n

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Landslide inventory and characteristics, based on LiDAR scanning and optimised field investigations in the Kutina area, Croatia<\/h5>\n

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Spatial distribution and geometric characteristics of landslides with special reference to geological units in the area of Slavonski Brod, Croatia<\/h5>\n

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Remote landslide mapping, field validation and model development \u2013 An example from Kravarsko, Croatia<\/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” width=”100%” custom_margin=”74px||36px||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/remote-landslide-mapping-field-validation-and-model-development-an-example-from-kravarsko-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=”117px|20px|20px|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″ 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

Multi-Level Sensing Technologies in Landslide Research\u2014Hrvatska Kostajnica Case Study, Croatia<\/h5>\n

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New insights into the earliest occurrence, possible evolutionary lineage, palaeogeography and palaeoclimatic implications of Nicklithus amplificus<\/em>: Evidence from the Adriatic Sea, Indian Ocean and Paratethys<\/span><\/h5>\n

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Ecotoxicological aspects related to the occurrence of emerging contaminants in the Dinaric karst aquifer of Jadro and \u017drnovnica springs<\/span><\/h5>\n

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Hydrogeological Assessment and Modified Conceptual Model of a Dinaric Karst Island Aquifer<\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/water_logo.png” alt=”water journal logo” title_text=”water_logo” _builder_version=”4.16″ _module_preset=”default” width=”100%” custom_margin=”84px||36px||false|false” custom_padding=”||0px|0px|false|false” global_colors_info=”{}”][\/et_pb_image][et_pb_button button_url=”https:\/\/www.hgi-cgs.hr\/hydrogeological-assessment-and-modified-conceptual-model-of-a-dinaric-karst-island-aquifer\/” 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=”140px|20px|20px|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

A Holocene Sedimentary Record and the Impact of Sea-Level Rise in the Karst Lake Velo Blato and the Wetlands on Pag Island (Croatia)<\/strong><\/h5>\n

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Emerging organic contaminants in karst groundwater: A global level assessment<\/span><\/h5>\n

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Revision of the endemic dinoflagellate cyst genus Pontiadinium<\/i> Stover & Evitt, 1978 from Lake Pannon and the Paratethys realm (Late Miocene\u2013Early Pliocene, Central Europe)<\/span><\/h5>\n

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

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NAJNOVIJI OBJAVLJENI RADOVILate Quaternary geomorphology and sedimentary processes in the Prolo\u0161ko Blato karst wetland (Imotsko Polje, Croatia) \u00a0Holocene paleoenvironmental changes recorded in the sediments of the karst Krka River estuary (eastern Adriatic coast, Croatia) \u00a0Defining the geological units susceptible to landslides in Pannonian Croatia using energy relief index\u00a0 \u00a0Croatian Critical Mineral Commodity Letters: Magnesium \u00a0Geochemical […]<\/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-36560","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/36560","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=36560"}],"version-history":[{"count":70,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/36560\/revisions"}],"predecessor-version":[{"id":45607,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/36560\/revisions\/45607"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=36560"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}