{"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":"2026-10-22T07:37:03","modified_gmt":"2026-10-22T07:37:03","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=”4.27.6″ custom_margin=”30px|auto||auto|false|false” custom_padding=”0px|0px|0px|0px|false|true” global_colors_info=”{}” theme_builder_area=”post_content”][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=”4.27.8″ 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|20px|29px|20px|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)” locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Identifying and naming non-pollen palynomorphs<\/span><\/strong><\/h5>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2026\/09\/clanak-1-logo.jpg” alt=”Geologia Croatica logo” title_text=”clanak 1 logo” disabled_on=”off|off|off” _builder_version=”4.27.8″ _module_preset=”default” width=”90%” custom_margin=”145px||-5px|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\/identifying-and-naming-non-pollen-palynomorphs\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.8″ 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|25px|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″ global_colors_info=”{}” custom_padding__hover=”|||” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.7″ 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|20px|29px|20px|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)” locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Reinvestigating the Zmajevac loess-palaesol sequence: A multi-proxy study of Late Pleistocene climate transitions in the southern Pannonian Basin<\/span><\/strong><\/h5>\n

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Aligning Croatia\u2019s National Solid Mineral Resources Classification System with UNFC: A Methodological Framework and Case-Based Implications<\/span><\/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=”4.27.9″ _module_preset=”default” width=”90%” custom_margin=”0px||-5px|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\/aligning-croatias-national-solid-mineral-resources-classification-system-with-unfc-a-methodological-framework-and-case-based-implications\/” button_text=”vidi vi\u0161e” button_alignment=”right” _builder_version=”4.27.7″ 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|25px|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″ global_colors_info=”{}” custom_padding__hover=”|||” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.27.7″ 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|20px|29px|20px|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)” locked=”off” global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

Mineralogical and Geochemical Variability of the Mamutovac-1a Upper Eocene Karst Bauxite Deposit (Croatian Dinarides) and Its CRM Potential<\/span><\/strong><\/h5>\n

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Evaluation of ERA5-Land Against Ground-Based Precipitation Observations in Supporting Landslide Analysis in Pannonian Croatia<\/h5>\n

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Middle Triassic ignimbrites as markers of Eoalpine high-pressure metamorphism and large-scale lateral extrusion of Adria derived units at the edge of the European Alps<\/h5>\n

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Geodynamic evolution of the Northernmost Dinarides revealed by the petrogenesis of Mid-Triassic calc-alkaline volcanic rocks<\/h5>\n

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Holocene Paleolake Evolution of the Bribir\u2013Ostrovica Karst Polje (Dalmatia, Croatia): A Multi-Proxy Lake Sediment Record<\/h5>\n

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Effects of Precipitation Trends, Extremes, and Antecedent Moisture Controls on Landslide Triggering in Hum na Sutli and Northern Croatia<\/h5>\n

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40<\/sup>Ar\/39<\/sup>Ar Ages of Glaucophane and Phengitic Muscovite from the Mt. Medvednica blueschists (NW Croatia): Evidence for Middle-Late Jurassic Subduction in the Northwestern\u00a0 Neotethys<\/strong>\u201d<\/h5>\n

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Geomorphological influence on the Holocene climate signal from a karst wetland in the Central Mediterranean<\/h5>\n
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Holocene paleoclimate reconstruction on the eastern Adriatic based on ostracods and stable isotopes from a coastal Lake Velo Blato (Croatia)<\/h5>\n
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Direct evidence of active tectonics along the offshore sector of the Dinaric Fault System<\/strong><\/h5>\n
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Remote Sensing and Multi-Level Data Analyses for Hum na Sutli Landslide Impact Assessment in a Changing Climate<\/strong><\/h5>\n
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Late Miocene to Pliocene Enigma in the SW Pannonian Basin System:
New cosmogenic nuclide dating indicates \u223c1 Myr earlier regression of Lake Pannon and basin inversion<\/strong><\/h5>\n
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Geozonation of the Zagreb city area as an input for seismic risk assessment<\/h5>\n
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Integrated approach for characterizing aquifer heterogeneity in alluvial plains<\/h5>\n
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Comparative Analysis of Slope and Relief Energy for Small-Scale Landslide Susceptibility Mapping: Insights from Croatia<\/h5>\n
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A comprehensive dataset of landslide inventory in Pannonian Croatia: Archived and reported data<\/h5>\n
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Eocene Weathering Oscillations Imprinted in Marl Mineral and Geochemical Record, Dinaric Foreland Basin, Croatia<\/h5>\n
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Late Quaternary geomorphology and sedimentary processes in the Prolo\u0161ko Blato karst wetland (Imotsko Polje, Croatia)<\/h5>\n
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Holocene paleoenvironmental changes recorded in the sediments of the karst Krka River estuary (eastern Adriatic coast, Croatia)<\/span><\/h5>\n
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Defining the geological units susceptible to landslides in Pannonian Croatia using energy relief index<\/em>\u00a0<\/span><\/h5>\n
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Croatian Critical Mineral Commodity Letters: Magnesium<\/h5>\n
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Geochemical Insights and Mineral Resource Potential of Rare Earth Elements (REE) in the Croatian Karst Bauxites<\/span><\/h5>\n
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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
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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 RADOVIIdentifying and naming non-pollen palynomorphsReinvestigating the Zmajevac loess-palaesol sequence: A multi-proxy study of Late Pleistocene climate transitions in the southern Pannonian BasinAligning Croatia\u2019s National Solid Mineral Resources Classification System with UNFC: A Methodological Framework and Case-Based ImplicationsMineralogical and Geochemical Variability of the Mamutovac-1a Upper Eocene Karst Bauxite Deposit (Croatian Dinarides) and Its CRM […]<\/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":[],"aioseo_head":"\n\t\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\n\t\t