{"id":33840,"date":"2020-09-18T10:40:30","date_gmt":"2020-09-18T10:40:30","guid":{"rendered":"http:\/\/www.hgi-cgs.hr\/?page_id=33840"},"modified":"2020-12-31T14:54:34","modified_gmt":"2020-12-31T14:54:34","slug":"geolosko-modeliranje","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/geolosko-modeliranje\/","title":{"rendered":"Geological Modeling"},"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=”4.7.7″ 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=”https:\/\/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=”https:\/\/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=”https:\/\/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=”https:\/\/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=”https:\/\/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=”https:\/\/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=”https:\/\/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_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.7.7″ 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” sticky_transition=”on”][\/et_pb_slide][et_pb_slide heading=”Hrvatski geolo\u0161ki institut” _builder_version=”4.7.7″ 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” sticky_transition=”on”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.4.2″ custom_padding=”20px||41px|||”][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.6.5″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_4_line_height=”1.3em”]<\/p>\n

TEMELJNA GEOLO\u0160KA ISTRA\u017dIVANJA<\/strong><\/h2>\n

Geolo\u0161ko modeliranje
<\/strong><\/h4>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”3.25″][et_pb_column type=”4_4″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.6.6″ custom_margin=”-14px|||||” custom_padding=”|10px||10px|false|true”]<\/p>\n

Geolo\u0161ko modeliranje je metoda koja obuhva\u0107a prikupljanje geolo\u0161kih podataka istra\u017eivanog podru\u010dja, njihovu interpretaciju i obradu te u kona\u010dnici izradu geolo\u0161kog modela.<\/p>\n

Geolo\u0161ki model je numeri\u010dka parametrizacija povr\u0161ine i podzemlja istra\u017eivanog podru\u010dja, koji se prikazuje trodimenzionalnim vizualizacijama.<\/p>\n

Ulazni podaci uklju\u010duju sve vrste prostornih podataka u rasterskom i vektorskom obliku te geolo\u0161ke, geofizi\u010dke i geotehni\u010dke podatke. Geolo\u0161ko modeliranje je proces koji podrazumijeva slo\u017eenu obradu i interpretaciju navedenih podataka u specijaliziranim ra\u010dunalnim programskim paketima, koji rezultira izradom 3D geolo\u0161kog modela. Modeli se koriste za dobivanje detaljnog uvida u geolo\u0161ke odnose i procese, kao \u0161to su prostorni raspored i orijentacija struktura, polo\u017eaj i arhitektura litofacijesa (stratigrafskih i litolo\u0161kih jedinica) te prostorno-vremenskih odnosa mehanizama i uvjeta talo\u017eenja (podaci o geodinamskim procesima) i drugo. Geolo\u0161ko modeliranje stoga zahtjeva interdisciplinarni pristup i znanja iz podru\u010dja geofizike, strukturne geologije, sedimentologije, stratigrafije, sekvencijalne stratigrafije, ali i iz ostalih polja geologije. Na Hrvatskom geolo\u0161kom institutu, geolo\u0161ko modeliranje provodi se na cjelokupnom podru\u010dju Republike Hrvatske, kao sastavni dio regionalnih i lokalnih temeljnih geolo\u0161kih istra\u017eivanja Zemljine kore. Uz \u010destu primjenu u znanstveno usmjerenim istra\u017eivanjima, geolo\u0161ki modeli su nezaobilazni i u primijenjenim istra\u017eivanjima:<\/p>\n

    \n
  • plitkih vodonosnika<\/li>\n
  • dubljih vodonosnika s geotermalnom vodom<\/li>\n
  • le\u017ei\u0161ta ugljikovodika<\/li>\n
  • podzemnih skladi\u0161ta energije, plinova i sli\u010dno.<\/li>\n<\/ul>\n

    Naj\u010de\u0161\u0107e kori\u0161teni ulazni podaci u geolo\u0161kom modeliranju:<\/p>\n

      \n
    • geofizi\u010dki podaci (2D refleksijska i refrakcijska seizmika, 3D refleksijska seizmika, karota\u017ena mjerenja u bu\u0161otinama, gravimetrijski i seizmolo\u0161ki podaci),<\/li>\n
    • bu\u0161otinski podaci (geolo\u0161ke i geotehni\u010dke interpretacije jezgre, \u201eMaster log\u201c),<\/li>\n
    • povr\u0161inski podaci (geolo\u0161ke karte, geolo\u0161ki profili, geolo\u0161ki stupovi, povr\u0161inska mjerenja itd.),<\/li>\n
    • prostorni podaci (GIS) u rasterskom (DEM, DMR, DTM, topografske karte, geolo\u0161ke i druge tematske karte, satelitske i avio snimke) i vektorskom obliku (geolo\u0161ke jedinice i granice, ceste, vodotoci),<\/li>\n
    • podaci prikupljeni daljinskim istra\u017eivanjima (obra\u0111eni fotogrametrijski, multispektralni, laserski i radarski podaci).<\/li>\n<\/ul>\n

      Programski paketi kori\u0161teni za geolo\u0161ko modeliranje: PetEx Move, akademska licenca Schlumberger Petrel, akademska licenca SKUA-GOCAD, akademska licenca Landmark DecisionSpace Geosciences.<\/p>\n

      Programski paketi kori\u0161teni za obradu podataka: ESRI ArcGIS, QuantumGIS, Adobe Illustrator, Corel.<\/p>\n

      [\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/geoterm-model.jpg” alt=”Geolo\u0161ki model zagreba\u010dkog geotermalnog vodonosnika (u izradi)” title_text=”geoterm model” url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/geoterm-model.jpg” align=”center” _builder_version=”4.6.6″ _module_preset=”default” width=”50%” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” width=”55%” module_alignment=”center” custom_margin=”-30px||||false|false”]<\/p>\n

      Geolo\u0161ki model zagreba\u010dkog geotermalnog vodonosnika (u izradi), s prikazanim povr\u0161inama krovine i podine vodonosnika te putanjama kanala bu\u0161otina, rezultat Radnog paketa 1 (WP1), projekta GeoTwinn.<\/p>\n

      [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_2,1_2″ _builder_version=”3.25″ custom_padding=”15px|0px|1px|0px|false|false”][et_pb_column type=”1_2″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/cicarija.jpg” alt=”geolo\u0161ki model \u0106i\u0107arije” title_text=”geolo\u0161ki model \u0106i\u0107arije” url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/cicarija.jpg” align=”right” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.6.6″ max_width=”89%” module_alignment=”right” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/cicarija2.jpg” alt=”geolo\u0161ki model \u0107i\u0107arije” title_text=”cicarija2″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/cicarija2.jpg” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.6.6″ width=”88%” max_width=”99%” module_alignment=”left” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.6.6″ _module_preset=”default” custom_padding=”||10px|||”][et_pb_column type=”4_4″ _builder_version=”4.6.6″ _module_preset=”default”][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” custom_margin=”-10px||||false|false”]<\/p>\n

      Geolo\u0161ki model \u0106i\u0107arije s prikazanom tipi\u010dnom navla\u010dnom strukturom krednih i paleogenskih naslaga vanjskih Dinarida (u izradi), rezultat Radnog paketa 1 (WP1), projekta GeoTwinn.<\/p>\n

      [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_2,1_2″ _builder_version=”3.25″ custom_padding=”15px|0px|40px|0px|false|false”][et_pb_column type=”1_2″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/zagreb.jpg” alt=”geolo\u0161ki model zagreba\u010dkog vodonosnika podzemen vode” title_text=”zagreb” url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/zagreb.jpg” align=”right” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.6.6″ max_width=”89%” module_alignment=”right” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” width=”100%” module_alignment=”center” custom_margin=”-30px||||false|false” custom_padding=”|||50px|false|false”]<\/p>\n

      Geolo\u0161ki model zagreba\u010dkog vodonosnika podzemne vode, s prikazanim klasti\u010dnim aluvijalnim naslagama vodonosnika i neogenskim stijenama u podlozi, rezultat Radnog paketa 1 (WP1), projekta GeoTwinn.<\/p>\n

      [\/et_pb_text][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/rms.png” alt=”Prikaz razdiobe okoli\u0161a talo\u017eenja kori\u0161tenjem RMS atributnih analiza refleksijskih seizmi\u010dkih podataka ” title_text=”rms” url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/rms.png” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.6.6″ width=”94%” max_width=”99%” module_alignment=”left” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” custom_padding=”|30px|||false|false”]<\/p>\n

      Prikaz razdiobe okoli\u0161a talo\u017eenja kori\u0161tenjem RMS atributnih analiza refleksijskih seizmi\u010dkih podataka na kartiranim stratigrafskim povr\u0161inama (kori\u0161teni program – Sclumberger Petrel u svrhu doktorskog istra\u017eivanja).<\/p>\n

      [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_2,1_2″ _builder_version=”3.25″ custom_padding=”15px|0px|40px|0px|false|false”][et_pb_column type=”1_2″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/potres.png” alt=”Geolo\u0161ki model dvije rasjedne plohe du\u017e kojih se nalaze hipocentri glavnog i popratnih potresa zabilje\u017eenih na \u0161irem zagreba\u010dkom podru\u010dju 22. o\u017eujka 2020.” title_text=”potres” url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/potres.png” align=”right” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.6.6″ width=”81%” max_width=”89%” module_alignment=”right” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” width=”100%” module_alignment=”center” custom_margin=”-30px||||false|false” custom_padding=”|||80px|false|false”]<\/p>\n

      Geolo\u0161ki model dvije rasjedne plohe du\u017e kojih se nalaze hipocentri glavnog i popratnih potresa zabilje\u017eenih na \u0161irem zagreba\u010dkom podru\u010dju 22. o\u017eujka 2020., izra\u0111en metodologijom razvijenom na projektu Geosekva.<\/p>\n

      [\/et_pb_text][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/3D-GEOSEKVA.gif” title_text=”3D GEOSEKVA” url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/3D-GEOSEKVA.gif” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.6.6″ max_width=”99%” module_alignment=”left” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px”][\/et_pb_image][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false”]<\/p>\n

      Prikaz kartirane povr\u0161ine na podru\u010dju sjevernog Jadrana (projekt GEOSEKVA, HRZZ).<\/p>\n

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

      TEMELJNA GEOLO\u0160KA ISTRA\u017dIVANJA Geolo\u0161ko modeliranje Geolo\u0161ko modeliranje je metoda koja obuhva\u0107a prikupljanje geolo\u0161kih podataka istra\u017eivanog podru\u010dja, njihovu interpretaciju i obradu te u kona\u010dnici izradu geolo\u0161kog modela. Geolo\u0161ki model je numeri\u010dka parametrizacija povr\u0161ine i podzemlja istra\u017eivanog podru\u010dja, koji se prikazuje trodimenzionalnim vizualizacijama. Ulazni podaci uklju\u010duju sve vrste prostornih podataka u rasterskom i vektorskom obliku te geolo\u0161ke, […]<\/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-33840","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