{"id":29866,"date":"2020-04-08T08:58:16","date_gmt":"2020-04-08T08:58:16","guid":{"rendered":"http:\/\/www.hgi-cgs.hr\/?page_id=29866"},"modified":"2020-10-21T12:59:53","modified_gmt":"2020-10-21T12:59:53","slug":"zavrseni-projekti-joint-u-s","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/zavrseni-projekti-joint-u-s\/","title":{"rendered":"Zavr\u0161eni projekti – Joint U.S."},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.4.1″ custom_padding=”0px||0px|||”][et_pb_fullwidth_slider _builder_version=”4.4.2″ min_height=”112px” height=”400px” custom_margin=”0px||||false|false” custom_padding=”0px||18px||false|false” auto=”on” auto_ignore_hover=”on” locked=”off”][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Br\u010di\u0107_Drvenik02-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban2-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.4.1″ header_font=”|||on|||||” background_image=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg” background_enable_image=”on” locked=”off” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.4.2″ text_font_size=”32px” header_2_text_color=”#1e5096″]<\/p>\n

ZAVOD ZA GEOLOGIJU<\/strong><\/h2>\n

Zavr\u0161eni projekti
<\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″ custom_padding=”21px|||||”][et_pb_row _builder_version=”3.25″ custom_margin=”-37px|auto||auto||” custom_padding=”||50px”][et_pb_column type=”4_4″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.4.2″ 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” min_height=”76px” custom_margin=”20px||0px||false|false” custom_padding=”||0px|||” 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)”]<\/p>\n

Joint U.S. \u2013 Croatian cooperative research project: Greenhouse and transitional <\/strong><\/h3>\n

climates in 50 m.y. carbonate record of the Late Jurassic \u2013 Early <\/strong><\/h3>\n

Cretaceous <\/strong>Dinaric Carbonate Platfrom <\/strong><\/h3>\n

[\/et_pb_text][et_pb_tabs _builder_version=”4.6.6″ custom_margin=”23px|||||” hover_enabled=”0″ sticky_enabled=”0″][et_pb_tab title=”O projektu” _builder_version=”4.6.5″]<\/p>\n

Projekt je imao za cilj istra\u017eiti pretpostavku da unutar gornjojursko-donjokrednog slijeda Jadranske platforme istalo\u017eenog tijekom klasi\u010dnog greenhouse klimatskog razdoblja, postoje dokazi o kra\u0107im razdobljima zahla\u0111enja tijekom kojih je dominirala glacioeustazija umjerenih amplituda, a \u0161to bi u kona\u010dnici upu\u0107ivalo na postojanje leda na visokim zemljopisnim \u0161irinama. U ostvarivanju ciljeva i potvr\u0111ivanja hipoteze projekta snimljeno je vi\u0161e kontinuiranih geolo\u0161kih stupova kroz srednjojursko-srednjokredne naslage, \u010dija ukupna analizirana debljina nadma\u0161uje planiranu. Istra\u017eivani lokaliteti ulju\u010duju: (1) Otok Hvar – detaljni litostratigrafski stup kroz aptsko-starijealbske naslage snimljen je u blizini naselja Jelsa; (2) Otok Kor\u010dula – na podru\u010dju \u010care i Pupnate snimljeno je pet litostratigrafskih supova koji obuvha\u0107aju raspon od barema do gornjeg alba; (3) Poluotok Pelje\u0161ac – snimljen je kra\u0107i slijed berijaskih dolomita, te du\u017ei profil kroz baremsko-aptske naslage; (4) Otok Mljet – \u010detiri litostratigrafska stupa snimljena su na podru\u010dju Sobre, Kozarica i Babinog Polja; (5) Dubrova\u010dko zale\u0111e – sedam kontinuiranih profila detaljno je istra\u017eeno na \u0161irem prostoru Jasenica, Brotnica i Velji do. Usporedno sa snimanjem detaljno su bili prikupljani uzorci vapnenaca za mikropaleontolo\u0161ko-biostratigrafsku i sedimentolo\u0161ko-petrografsku analitiku (uklju\u010duju\u0107i katodoluminescenciju), te vapnanaca i dolomita za analizu stabilnih izotopa i elemenata u tragovima. Rezultati spektralne analize ciklo- i kemostratigrafije upu\u0107uju na dominantan utjecaj ekscentri\u010dnosti zemljine orbite (ciklusi od 100.000 i 400.000 godina) na oscilacije morske razine tijekom donje krede. Rezultati tako\u0111er upu\u0107uju da unutar istra\u017eivanog slijeda Jadranske platforme kemostratigrafski signal nije u potpunosti o\u010duvan.<\/p>\n

[\/et_pb_tab][et_pb_tab title=”Voditelj” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Glavni istra\u017eiva\u010d \/ voditelj:\u00a0<\/span><\/em><\/strong><\/p>\n

dr.sc. Valentina Hajek – Tadesse <\/em><\/p>\n

dr.sc. Antun Husinec (St. Lawrence University)<\/em><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Suradnici” _builder_version=”4.6.5″]<\/p>\n

Bo\u017eo Prtoljan, <\/span><\/p>\n

Damir Palenik, <\/span><\/p>\n

Antun Husinec (St. Lawrence University), <\/span><\/p>\n

Fred Read (Virginia Tech), <\/span><\/p>\n

Sean Regan (St. Lawrence University), <\/span><\/p>\n

David Mosher (St. Lawrence University)<\/span><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Trajanje projekta” _builder_version=”4.6.5″]<\/p>\n

Datum po\u010detka i kraja projekta: <\/strong>2008-2011<\/span><\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Kategorija” _builder_version=”4.6.5″]<\/p>\n

Kategorija projekta:<\/strong>\u00a0<\/span><\/span>Bilateralni projekt (znanstveno-istra\u017eiva\u010dka suradnja SAD (National Science Foundation)-Hrvatska (MZO\u0160 RH))<\/span><\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Iznos financiranja” _builder_version=”4.6.5″]<\/p>\n

Ugovoreni iznos financiranja:<\/strong> <\/span>166.500,00 kn<\/span><\/p>\n

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[\/et_pb_tab][et_pb_tab title=”Status” _builder_version=”4.6.5″]<\/p>\n

Status:<\/strong> Zavr\u0161en<\/span><\/p>\n

[\/et_pb_tab][\/et_pb_tabs][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"

ZAVOD ZA GEOLOGIJU Zavr\u0161eni projekti Joint U.S. \u2013 Croatian cooperative research project: Greenhouse and transitional climates in 50 m.y. carbonate record of the Late Jurassic \u2013 Early Cretaceous Dinaric Carbonate Platfrom Projekt je imao za cilj istra\u017eiti pretpostavku da unutar gornjojursko-donjokrednog slijeda Jadranske platforme istalo\u017eenog tijekom klasi\u010dnog greenhouse klimatskog razdoblja, postoje dokazi o kra\u0107im razdobljima […]<\/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-29866","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