{"id":43184,"date":"2024-03-04T13:24:42","date_gmt":"2024-03-04T13:24:42","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=43184"},"modified":"2025-01-23T09:35:32","modified_gmt":"2025-01-23T09:35:32","slug":"geoloska-evolucija-sinorogenetskih-i-postorogenetskih-taloznih-sustava-otoka-raba-i-krka-gorik","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/geoloska-evolucija-sinorogenetskih-i-postorogenetskih-taloznih-sustava-otoka-raba-i-krka-gorik\/","title":{"rendered":"Geolo\u0161ka evolucija sinorogenetskih i postorogenetskih talo\u017enih sustava otoka Raba i Krka (GORIK)"},"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=”||7px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ 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

\u00a0<\/strong><\/h2>\n

INTERNI ISTRA\u017dIVA\u010cKI PROJEKTI
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[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”5px||41px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ custom_margin=”||20px” custom_padding=”||50px” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ custom_padding=”|||” global_colors_info=”{}” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.24.0″ text_font=”|300|||||||” ul_font=”||||||||” header_font=”||||||||” header_text_align=”center” header_2_font=”|800|||||||” header_2_text_align=”center” header_2_text_color=”#1e5096″ header_2_font_size=”54px” header_3_font=”|300|||||||” header_3_line_height=”1.3em” text_orientation=”center” custom_margin=”-4px||18px|||” custom_padding=”||22px|||” animation_direction=”bottom” header_2_font_size_tablet=”” header_2_font_size_phone=”30px” header_2_font_size_last_edited=”on|phone” header_2_text_shadow_style=”preset1″ header_2_text_shadow_horizontal_length=”0.03em” header_2_text_shadow_vertical_length=”0.03em” header_2_text_shadow_blur_strength=”0.05em” header_2_text_shadow_color=”rgba(0,0,0,0.3)” global_colors_info=”{}”]<\/p>\n

“Geolo\u0161ka evolucija sinorogenetskih i postorogenetskih talo\u017enih sustava otoka Raba i Krka\u201c (GORIK) <\/strong><\/h3>\n

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[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2025\/01\/GORIK_logo-01.jpg” _builder_version=”4.27.4″ _module_preset=”default” title_text=”GORIK_logo-01″ width=”17%” module_alignment=”center” custom_padding=”||20px||false|false” hover_enabled=”0″ sticky_enabled=”0″][\/et_pb_image][et_pb_tabs _builder_version=”4.24.0″ custom_margin=”-15px||||false|false” global_colors_info=”{}”][et_pb_tab title=”O projektu” _builder_version=”4.24.0″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

Cilj projekta GORIK je istra\u017eivanje utjecaja tektonike na stvaranje i evoluciju sin- i postorogenetskih talo\u017enih bazena na podru\u010dju otoka Raba i Krka. Sinorogenetske naslage paleogena dio su pojasa koji se pru\u017ea sjeverozapad \u2013 jugoistok, du\u017e isto\u010dne obale Jadranskog mora. Tijekom paleogena su, uslijed orogenetskih procesa, formirani dinarski predgorski bazeni u kojima su istalo\u017eene naslage koje sadr\u017ee vrijedan zapis o tektonskoj evoluciji Perijadranskog (Dinarskog) prostora. Tektonske faze koje su se odvijale tijekom paleogena, kao i sam prostorni raspored te sastav paleogenskih naslaga, imali su zna\u010dajan utjecaj na geolo\u0161ku i strukturnu gra\u0111u. U cilju boljeg i suvremenijeg razumijevanja tektonske evolucije prostora pristupit \u0107e se istra\u017eivanju paleogenskih naslaga kroz detaljne strukturne, sedimentolo\u0161ke i paleontolo\u0161ke analize te geolo\u0161ko kartiranje. Kartiranjem \u0107e se, osim navedenih naslaga, obuhvatiti i karbonatne naslage talo\u017eene na mezozojskoj karbonatnoj platformi, \u0161to je nu\u017eno za razumijevanje \u0161ireg strukturnog sklopa. Nadalje, istra\u017eivanjima \u0107e se obuhvatiti i kvartarni sedimenti koji sadr\u017ee zapise o postorogenetskim doga\u0111ajima, a koji su vezani uz promjene klime i oscilacije razine mora tijekom kvartara. Rezultati istra\u017eivanja bit \u0107e objavljeni u znanstvenim publikacijama te kao list Osnovne geolo\u0161ke karte RH M 1:50.000 otoka Raba, koja je ujedno i nu\u017ena osnova za sva daljnja usmjerena primijenjena i znanstvena geolo\u0161ka istra\u017eivanja.<\/span><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Voditelj” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Glavni istra\u017eiva\u010d \/ voditelj projekta:<\/strong><\/em> dr. sc. Kre\u0161imir Petrinjak<\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Suradnici” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Hrvatski geolo\u0161ki institut, Zagreb:<\/strong><\/p>\n

Ladislav Fu\u010dek,<\/p>\n

Tvrtko Korbar,<\/p>\n

Lara Wacha,<\/p>\n

Damir Palenik,<\/p>\n

Tomislav Kure\u010di\u0107,<\/p>\n

Marko Budi\u0107,<\/p>\n

Stanislav Bergant,<\/p>\n

Jelena \u0160pani\u010dek<\/p>\n

 <\/p>\n

Rudarsko-geolo\u0161ko-naftni fakultet, Zagreb:<\/strong><\/p>\n

Igor Vlahovi\u0107,<\/p>\n

Bojan Mato\u0161,<\/p>\n

Darko Mate\u0161i\u0107<\/p>\n

[\/et_pb_tab][et_pb_tab title=”Trajanje projekta” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Trajanje projekta:<\/strong> 01.01.2024.\u201331.12.2027.<\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Kategorija” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Kategorija projekta: <\/strong><\/span>istra\u017eiva\u010dki projekt pra\u0107en od strane Ministarstva znanosti i obrazovanja Republike Hrvatske; sredstva iz Nacionalnog plana oporavka i otpornosti 2021.\u20132026. \u2013 NextGenerationEU<\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Iznos financiranja” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

Financiranje:\u00a0<\/strong><\/em>60,825.00 \u20ac\u00a0<\/p>\n

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    [\/et_pb_tab][et_pb_tab title=”Status” _builder_version=”4.24.0″ global_colors_info=”{}”]<\/p>\n

    Status:<\/strong> Aktivan<\/em><\/span><\/p>\n

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    \u00a0 INTERNI ISTRA\u017dIVA\u010cKI PROJEKTI”Geolo\u0161ka evolucija sinorogenetskih i postorogenetskih talo\u017enih sustava otoka Raba i Krka\u201c (GORIK) Cilj projekta GORIK je istra\u017eivanje utjecaja tektonike na stvaranje i evoluciju sin- i postorogenetskih talo\u017enih bazena na podru\u010dju otoka Raba i Krka. Sinorogenetske naslage paleogena dio su pojasa koji se pru\u017ea sjeverozapad \u2013 jugoistok, du\u017e isto\u010dne obale Jadranskog mora. Tijekom […]<\/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-43184","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