{"id":43158,"date":"2024-02-28T06:10:51","date_gmt":"2024-02-28T06:10:51","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=43158"},"modified":"2025-02-27T08:11:40","modified_gmt":"2025-02-27T08:11:40","slug":"interni-istrazivacki-projekti","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/interni-istrazivacki-projekti\/","title":{"rendered":"Internal Research Projects"},"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_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.16″ header_font=”|||on|||||” background_image=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/04\/20191015_142016a-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\/04\/20191014_133538-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″ global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ custom_margin=”21px|auto||auto||” custom_padding=”||11px|||” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_text _builder_version=”4.24.0″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}”]<\/p>\n

INTERNI ISTRA\u017dIVA\u010cKI PROJEKTI
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BAKA<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Osnovna hidrogeolo\u0161ka karta Baranje<\/strong><\/em><\/a><\/h6>\n
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DONA<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Dinamika ogolina Istre: od uzorka do sliva<\/a> <\/em><\/h6>\n
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GEACAP<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Globalni doga\u0111aji u naslagama Jadranske karbonatne platforme<\/strong><\/em><\/a><\/h6>\n
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GeoDRIFT<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Geodinamska evolucija dinaridskih riftnih bazena u srednjem trijasu<\/em> <\/strong><\/a><\/h6>\n
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GeoSAVAGE<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Geolo\u0161ka evolucija Zapadnog Savskog bazena \u2013 Starosti i Geodinamika (GeoSAVAGE)<\/strong><\/em><\/a><\/h6>\n
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GORIK<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Geolo\u0161ka evolucija sinorogenetskih i postorogenetskih talo\u017enih sustava otoka Raba i Krka<\/strong><\/em><\/a><\/h6>\n
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GRGA<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Paleookoli\u0161na i paleoklimatska istra\u017eivanja klasti\u010dnih i kemogenih sedimenata iz Grgosovih spilja<\/strong><\/em><\/a><\/h6>\n
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NITROVERT<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Ciklus du\u0161ika i prihranjivanje podzemne vode kroz vadoznu zonu u vodonosnicima s me\u0111uzrnskom poroznosti <\/em><\/a><\/h6>\n
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NONa<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Istra\u017eivanje kr\u0161kog vodonosnika nizvodno od Ogulina uz primjenu “novih” one\u010di\u0161\u0107ivala <\/strong><\/em><\/a><\/h6>\n
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PAPER CLICHE<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Reakcija pliocenskog i pleistocenskog okoli\u0161a na klimatske promjene<\/em><\/a><\/h6>\n
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PAPUKRON<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Komplementarna petrokronolo\u0161ka karakterizacija granita, progresivno metamorfnih stijena i migmatita u metamorfnom kompleksu Papuka (Slavonske planine, Hrvatska)<\/strong><\/em><\/a><\/h6>\n
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[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.24.2″ _module_preset=”default” global_colors_info=”{}” sticky_enabled=”0″ hover_enabled=”0″][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/02\/PLATE_final.jpg” title_text=”PLATE_final” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″ force_fullwidth=”on”][\/et_pb_image][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” header_4_text_color=”#1e5096″ header_6_text_color=”#666666″ header_6_font_size=”13px” custom_margin=”80px||||false|false” hover_enabled=”0″ global_colors_info=”{}” admin_label=”Text” sticky_enabled=”0″]<\/p>\n

PLATE<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Paleolimnologija hrvatskih kr\u0161kih jezera: pra\u0107enje promjena okoli\u0161a <\/strong><\/em><\/a><\/h6>\n
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RIM<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Rivers Into MAD: Odre\u0111ivanje paleookoli\u0161a rijeka Jadra i Cetine tijekom posljednjeg glacijalnog maksimuma<\/strong><\/em><\/a><\/h6>\n
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RAMPA<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Razvoj miocenskih paleookoli\u0161a na prostoru Hrvatske i njihova povezanost s globalnim doga\u0111ajima <\/strong><\/em><\/a><\/h6>\n
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SIS-VIS<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Sistematizacija postoje\u0107ih podataka, finalizacija istra\u017eivanja i izrada Osnovne hidrogeolo\u0161ke karte otoka Visa (SIS-VIS)<\/strong><\/em><\/a><\/h6>\n
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WEGETA<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>WEathering and VEGETAtion intertwined \u2014 multiproxy approach to understand the fate of terrestrial ecosystems in times of global climate change <\/strong><\/em><\/a><\/h6>\n
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ZG-LAB<\/strong><\/span><\/h4>\n
<\/em><\/strong><\/em><\/strong>Opremanje Laboratorija Zavoda za Geologiju<\/strong><\/em><\/a><\/h6>\n
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[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][\/et_pb_column][et_pb_column type=”1_4″ _builder_version=”4.16″ global_colors_info=”{}”][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"

INTERNI ISTRA\u017dIVA\u010cKI PROJEKTIBAKA Osnovna hidrogeolo\u0161ka karta Baranje DONA Dinamika ogolina Istre: od uzorka do sliva GEACAP Globalni doga\u0111aji u naslagama Jadranske karbonatne platforme GeoDRIFT Geodinamska evolucija dinaridskih riftnih bazena u srednjem trijasu GeoSAVAGE Geolo\u0161ka evolucija Zapadnog Savskog bazena \u2013 Starosti i Geodinamika (GeoSAVAGE) GORIK Geolo\u0161ka evolucija sinorogenetskih i postorogenetskih talo\u017enih sustava otoka Raba i Krka […]<\/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-43158","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