{"id":33199,"date":"2020-09-08T10:28:56","date_gmt":"2020-09-08T10:28:56","guid":{"rendered":"http:\/\/www.hgi-cgs.hr\/?page_id=33199"},"modified":"2020-10-15T11:30:39","modified_gmt":"2020-10-15T11:30:39","slug":"qmad-porijeklo-i-talozenje-sedimenata-u-vrijeme-kasno-kvartarnih-promjena-morske-razine-sustav-rijeke-krke-i-srednjojadranske-kotline","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/qmad-porijeklo-i-talozenje-sedimenata-u-vrijeme-kasno-kvartarnih-promjena-morske-razine-sustav-rijeke-krke-i-srednjojadranske-kotline\/","title":{"rendered":"QMAD &#8211; Porijeklo i talo\u017eenje sedimenata u vrijeme kasno kvartarnih promjena morske razine: Sustav rijeke Krke i Srednjojadranske kotline"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; fullwidth=&#8221;on&#8221; _builder_version=&#8221;4.4.1&#8243; custom_padding=&#8221;0px||0px|||&#8221;][et_pb_fullwidth_slider _builder_version=&#8221;4.4.2&#8243; min_height=&#8221;112px&#8221; height=&#8221;400px&#8221; 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header_font=&#8221;|||on|||||&#8221; background_image=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/20190228_094232-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban3-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/Bijele_stijene-Gorski_kotar-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban4-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][et_pb_slide heading=&#8221;Hrvatski geolo\u0161ki institut&#8221; _builder_version=&#8221;4.4.1&#8243; header_font=&#8221;|||on|||||&#8221; background_image=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/03\/ban5-scaled.jpg&#8221; background_enable_image=&#8221;on&#8221; locked=&#8221;off&#8221; sticky_transition=&#8221;on&#8221;][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_row _builder_version=&#8221;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.6.1&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\"><strong>NOVOSTI<\/strong><\/h2>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.4.2&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_text _builder_version=&#8221;4.6.1&#8243; text_font_size=&#8221;32px&#8221; header_2_text_color=&#8221;#1e5096&#8243; header_2_line_height=&#8221;1.3em&#8221;]<\/p>\n<h2 style=\"text-align: center; color: #1e5096;\">QMAD &#8211; Porijeklo i talo\u017eenje sedimenata u vrijeme kasno kvartarnih promjena morske razine: Sustav rijeke Krke i Srednjojadranske kotline<\/h2>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.4.2&#8243; custom_padding=&#8221;20px||41px|||&#8221;][et_pb_row _builder_version=&#8221;4.4.2&#8243; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.4.2&#8243;][et_pb_image src=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/09\/logo_qmad2.jpg&#8221; title_text=&#8221;logo_qmad2&#8243; align=&#8221;center&#8221; align_tablet=&#8221;center&#8221; align_phone=&#8221;&#8221; align_last_edited=&#8221;on|desktop&#8221; _builder_version=&#8221;4.6.1&#8243; max_width=&#8221;30%&#8221; module_alignment=&#8221;center&#8221;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.0.3&#8243; min_height=&#8221;192px&#8221; custom_margin=&#8221;12px|auto||auto||&#8221; custom_padding=&#8221;0px|||||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.0.3&#8243;][et_pb_text _builder_version=&#8221;4.6.5&#8243; text_font=&#8221;||||||||&#8221; link_font=&#8221;||||||||&#8221; link_text_color=&#8221;#e09900&#8243; custom_margin=&#8221;18px|||||&#8221; custom_padding=&#8221;|10px||10px|false|true&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p style=\"text-align: left;\"><strong> Financiranje:<\/strong><em> Hrvatska zaklada za znanost<\/em><strong><br \/> Broj projekta:<\/strong><em> IP-04-2019-8505<\/em><strong><br \/> Vrsta:<\/strong><em> Istra\u017eiva\u010dki projekt<\/em><strong><br \/> Trajanje:<\/strong><em> 4 godine<\/em><strong><br \/> Po\u010detak:<\/strong><em> 1. prosinac 2019.<\/em><strong><br \/> Vrijednost financiranja:<\/strong><em> 1.040.000,00 kn<\/em><strong><br \/> Voditelj:<\/strong><em> dr. sc. Slobodan Miko<\/em><strong><\/strong><\/p>\n<p style=\"text-align: left;\">\n<div style=\"text-align: justify;\">\n<p style=\"text-align: left;\"><strong>Sa\u017eetak:<\/strong><\/p>\n<p style=\"text-align: left;\">Predlo\u017eeni projekt ima za cilj unaprijediti spoznaje do sada slabo istra\u017eene potopljene krajolike isto\u010dno-jadranskog \u0161elfa, kao i kasno-kvartarnih sedimenata istalo\u017eenih du\u017e isto\u010dnog dijela Srednjojadranske kotline (MAD, Jabu\u010dka kotlina). Istra\u017eivanje pleistocenske naplavne ravnice rijeke Krke dati \u0107e uvid u stratigrafski slijed sedimenata s razvojem deltnog sustava i estuarija, koji su nastali interakcijom eustatskih promjena razine mora i lokalnih faktora poput donosa sedimenata i tektonske aktivnosti. Kontinuirana morska sedimentacija tijekom kasnog kvartara, te donos materijala iz slivnog podru\u010dja rijeke Krke, biti \u0107e istra\u017een na prostoru isto\u010dnog dijela MAD-a. Primjenom geofizi\u010dkih metoda visoke rezolucije, te sedimentolo\u0161kih, petrofizi\u010dkih, geokemijskih, mikropaleontolo\u0161kih i aDNA metoda na uzorcima iz jezgara sedimenata, po prvi puta \u0107e se mo\u0107i pratiti paleookoli\u0161na evolucija od rije\u010dnih\/jezerskih do dubljemorskih okoli\u0161a na profilu kra\u0107em od 100 km (od jezera Prokljan u estuariju rijeke Krke do isto\u010dnog MAD-a). Prepoznat \u0107e se odgovaraju\u0107i klimatski i okoli\u0161ni pokazatelji, te \u0107e se dobiti uvid u migraciju i okoli\u0161nu prilagodbu lovaca i sakuplja\u010da koji su tijekom kasnog paleolitika obitavali na isto\u010dnoj obali Jadrana, gdje je vjerojatno postojala naplavna ravnica rijeke Krke. Dobiveni rezultati o promjenama morske razine i krajolika omogu\u0107it \u0107e razumijevanje mogu\u0107e interakcije me\u0111u ljudima sa \u0161ireg istra\u017eivanog prostora u vrijeme sustavnih traktova padaju\u0107e, niske i rastu\u0107e razine mora. Time \u0107e se istra\u017eiti mogu\u0107a uloga rijeke Krke kao kopnenog\/naplavnog \u201emosta\u201c za ljudsku migraciju. Posebna pa\u017enja bit \u0107e posve\u0107ena procjeni recentne brzine sedimentacije, prepoznavanju obilje\u017eja potopljenih krajolika, te tako\u0111er izra\u010dunu brzine akumulacije organskog ugljika i kopnenih komponenata sedimenata, te potencijalno toksi\u010dnih elemenata.<\/p>\n<\/div>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221; custom_padding=&#8221;||4px|||&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221;][et_pb_image src=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/09\/podrucje-istrazivanja1.jpg&#8221; title_text=&#8221;podrucje istrazivanja1&#8243; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221; width=&#8221;55%&#8221; module_alignment=&#8221;center&#8221;][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; column_structure=&#8221;1_2,1_2&#8243;][et_pb_column _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; type=&#8221;1_2&#8243;][et_pb_text _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; text_font_size=&#8221;13px&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243; custom_margin=&#8221;-20px||||false|false&#8221;]<\/p>\n<p style=\"text-align: right;\">Podru\u010dje istra\u017eivanja &#8211; obala prije 11000 godina<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; type=&#8221;1_2&#8243;][et_pb_text _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; text_font_size=&#8221;13px&#8221; module_alignment=&#8221;left&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243; custom_margin=&#8221;-20px||||false|false&#8221;]<\/p>\n<p>Podru\u010dje istra\u017eivanja &#8211; obala prije 20000 godina<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=&#8221;1_2,1_2&#8243; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221;][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221;][et_pb_image src=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/09\/geofizicka_istr.jpg&#8221; title_text=&#8221;geofizicka_istr&#8221; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221;][\/et_pb_image][et_pb_text _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; text_font_size=&#8221;13px&#8221; custom_margin=&#8221;-35px||||false|false&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p style=\"text-align: center;\">Geofizi\u010dka snimanja podmorja<\/p>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221;][et_pb_image src=&#8221;http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/09\/istr_busenja.jpg&#8221; title_text=&#8221;istr_busenja&#8221; _builder_version=&#8221;4.6.1&#8243; _module_preset=&#8221;default&#8221; width=&#8221;95%&#8221;][\/et_pb_image][et_pb_text _builder_version=&#8221;4.6.5&#8243; _module_preset=&#8221;default&#8221; text_font_size=&#8221;13px&#8221; custom_margin=&#8221;-35px||||false|false&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p style=\"text-align: center;\">Istra\u017ena bu\u0161enja\/jezgrovanje kvartarnih sedimenata podmorja\/jezera<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>NOVOSTIQMAD &#8211; Porijeklo i talo\u017eenje sedimenata u vrijeme kasno kvartarnih promjena morske razine: Sustav rijeke Krke i Srednjojadranske kotline Financiranje: Hrvatska zaklada za znanost Broj projekta: IP-04-2019-8505 Vrsta: Istra\u017eiva\u010dki projekt Trajanje: 4 godine Po\u010detak: 1. prosinac 2019. Vrijednost financiranja: 1.040.000,00 kn Voditelj: dr. sc. Slobodan Miko Sa\u017eetak: Predlo\u017eeni projekt ima za cilj unaprijediti spoznaje do [&hellip;]<\/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-33199","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/33199","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=33199"}],"version-history":[{"count":3,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/33199\/revisions"}],"predecessor-version":[{"id":35535,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/33199\/revisions\/35535"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=33199"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}