[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″ global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}”][et_pb_text _builder_version=”4.23.4″ text_font_size=”32px” header_2_text_color=”#1e5096″ hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_margin=”-18px|||||” custom_padding=”20px||41px|||” global_colors_info=”{}”][et_pb_row _builder_version=”4.16″ custom_margin=”-18px|auto|20px|auto||” 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=”4.16″ 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|||||||” text_orientation=”center” custom_margin=”-1px||18px|||” custom_padding=”0px||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)” global_colors_info=”{}”]<\/p>\n
[\/et_pb_text][et_pb_tabs _builder_version=”4.16″ custom_margin=”-27px|||||” global_colors_info=”{}”][et_pb_tab title=”O projektu” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n
Javna ustanova Nacionalni park Krka i Hrvatski geolo\u0161ki institut ugovorili su 2019. godine provo\u0111enje dvogodi\u0161njeg projekta \u201ePaleolimnolo\u0161ko istra\u017eivanje u NP \u201eKrka\u201c \u2013 Visova\u010dko jezero\u201c. Istra\u017eivanje \u0107e se provoditi u svrhu prou\u010davanja razvoja jezerskog sustava Visova\u010dko jezero od Ro\u0161kog slapa do Skradinskog buka u smislu geneze jezera, promjene u sedimentaciji koje ukazuju na promjene klimatskih uvjeta, promjena u kori\u0161tenju zemlji\u0161ta, erozije i paleohidrologije.<\/p>\n
U prvoj fazi provedena su geofizi\u010dka istra\u017eivanja koja su obuhvatila snimanje dna vi\u0161esnopnim dubinomjerom (multibeam echosounder, MB) i panoramskim dubinomjerom (side-scan sonar, SSS) te podpovr\u0161ine geolo\u0161kim dubinomjerom (sub-bottom profiler, SBP) i radarom za promatranje ispod povr\u0161ine zemlje (ground penetrating radar, GPR). Ova istra\u017eivanja do sada nisu provedena u NP Krka, a va\u017ena su osnova za sva dalja istra\u017eivanja. Za snimanje podpovr\u0161ine kori\u0161teni su SBP Innomar SES-2000 light i GPR MAL\u00c5 GX 80 u suradnji s tvrtkama Geomar d.o.o. Split i GeoDa consulting d.o.o.<\/p>\n
Mjerenjem dubine na istra\u017eivanom podru\u010dju s vi\u0161esnopnim dubinomjerom (MB WASSP S3) izra\u0111ena je detaljna batimetrijska karta Visova\u010dkog jezera te morfolo\u0161ka karta dna jezera. Prosje\u010dna dubina iznosila je -4 do -26 m, a najve\u0107a dubina -40 m Prvi podaci ukazuju na debljinu rije\u010dnih i jezerskih sedimenata ve\u0107u od 35 m, a vidljive su i brojne potopljene i zatrpane sedrene barijere i potopljene ponikve.<\/p>\n
Druga faza istra\u017eivanja ve\u0107 je zapo\u010dela bu\u0161enjem sedimenata klipnim jezgrilom na pet lokacija. Sedimenti iz prikupljenih jezgara (duljine do 8,4 m) \u0107e se analizirati sedimentolo\u0161kim, geokemijsko-mineralo\u0161kim i mikropaleontolo\u0161kim metodama.<\/p>\n
[\/et_pb_tab][et_pb_tab title=”Voditelj” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n
Glavni istra\u017eiva\u010d \/ voditelj: <\/span><\/em><\/strong>dr.sc. Nikolina Ilijani\u0107<\/em> [\/et_pb_tab][et_pb_tab title=”Suradnici” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n Slobodan Miko, <\/span><\/p>\n Ozren Hasan, <\/span><\/p>\n Dea Brunovi\u0107, <\/span><\/p>\n Martina \u0160parica Miko, <\/span><\/p>\n Ana Maria Heski,<\/span><\/p>\n Koraljka Bakra\u010d, <\/span><\/p>\n Hajek Tadesse, <\/span><\/p>\n Tamara Markovi\u0107, <\/span><\/p>\n Sa\u0161a Mesi\u0107, <\/span><\/p>\n Ivan Razum<\/span><\/p>\n [\/et_pb_tab][et_pb_tab title=”Trajanje projekta” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n Datum po\u010detka i kraja projekta:\u00a0<\/strong> <\/span>01.03.2019.-01.03.2021.<\/span><\/p>\n \u00a0<\/span><\/p>\n [\/et_pb_tab][et_pb_tab title=”Kategorija” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n Kategorija projekta:\u00a0<\/strong> <\/span>Znanstveno-istra\u017eiva\u010dki projekt (Javna ustanova Nacionalni park Krka)<\/span><\/p>\n [\/et_pb_tab][et_pb_tab title=”Iznos financiranja” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n Ugovoreni iznos financiranja: <\/strong>312.000,00 HRK<\/span><\/p>\n [\/et_pb_tab][et_pb_tab title=”Status” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n Status:<\/strong> Aktivan<\/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 MINERALNE SIROVINE IMARINSKU GEOLOGIJU Gospodarstveni (tr\u017ei\u0161ni) projektiPaleolimnolo\u0161ka istra\u017eivanja u NP Krka – Visova\u010dko jezero Javna ustanova Nacionalni park Krka i Hrvatski geolo\u0161ki institut ugovorili su 2019. godine provo\u0111enje dvogodi\u0161njeg projekta \u201ePaleolimnolo\u0161ko istra\u017eivanje u NP \u201eKrka\u201c \u2013 Visova\u010dko jezero\u201c. Istra\u017eivanje \u0107e se provoditi u svrhu prou\u010davanja razvoja jezerskog sustava Visova\u010dko jezero od Ro\u0161kog slapa […]<\/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-30756","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
<\/em><\/strong> <\/span><\/em><\/strong> <\/em><\/strong><\/p>\n
<\/span><\/p>\n
<\/span><\/p>\n
<\/span><\/p>\n