{"id":29040,"date":"2020-04-04T10:21:29","date_gmt":"2020-04-04T10:21:29","guid":{"rendered":"http:\/\/www.hgi-cgs.hr\/?page_id=29040"},"modified":"2020-12-31T14:51:29","modified_gmt":"2020-12-31T14:51:29","slug":"sedimentologija-mineralogija-i-petrologija-sedimentnih-stijena","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/sedimentologija-mineralogija-i-petrologija-sedimentnih-stijena\/","title":{"rendered":"Sedimentology, Mineralogy of Sedimentary rocks"},"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″][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.4.7″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_4_line_height=”1.3em” custom_margin=”||-11px|||”]<\/p>\n

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

Sedimentologija, mineralogija i petrologija sedimentnih stijena
<\/strong><\/h4>\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_margin=”-13px|||||” custom_padding=”20px||41px|||”][et_pb_row _builder_version=”3.25″ custom_margin=”-6px|auto||auto||”][et_pb_column type=”4_4″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.6.6″]<\/p>\n

U Zavodu za geologiju provode se sedimentolo\u0161ka istra\u017eivanja koja izu\u010davaju mehanizme i uvjete talo\u017eenja klasti\u010dnih, karbonatnih, evaporitnih i silicijskih sedimentnih stijena te njihove teksturno-strukturne, petrolo\u0161ke, mineralo\u0161ke, litofacijesne, biofacijesne, kemijske, biokemijske, paleontolo\u0161ke, litostratigrafske, paleogeografske i ekolo\u0161ke karakteristike i odlike. Istra\u017eivanja se temelje na terenskim i analiti\u010dkim tehnikama (opti\u010dka mikroskopija, XRD, TGA\/DSC, SEM-EDS).<\/p>\n

Ova istra\u017eivanja va\u017ena su zbog rekonstrukcija sedimentnih tijela i analiza facijesa, te su jedan od osnovnih alata definicije pojedinih litostratigrafskih jedinica u vremenu i prostoru, a samim time i baza za izradu osnovnih geolo\u0161kih te raznih namjenskih karata.<\/p>\n

Sedimentne stijene su najrasprostranjenija vrsta stijena u Hrvatskoj. One predstavljaju glavne vodonosnike i kolektorske stijene nafte i plina. Znanje o njihovom sastavu, karakteristikama i genezi sedimentnih tijela osobito su bitna u primijenjenoj geologiji pri istra\u017eivanju zaliha mineralnih sirovina, preveniranju i saniranju geohazarda te u potrazi za vodonosnicima.<\/p>\n

Dvoje djelatnika Zavoda za geologiju sudjeluju na istra\u017eiva\u010dkom HRZZ projektu sedimentolo\u0161ke tematike SEDBAS (Talo\u017eni paleobazeni, vodeni prolazi i migracije biote; Sedimentary paleobasins, water corridors and biota migrations)<\/a> voditelja prof. dr. sc. Marijana Kova\u010di\u0107a (PMF)<\/em>.<\/p>\n

Tako\u0111er trenutno sudjelujemo i na istra\u017eiva\u010dkom HRZZ projektu BREEMECO – Dinaridski predgorski bazen izme\u0111u dva eocenska terminalna optimuma: mogu\u0107i scenarij za sjevernojadranski bazen<\/a><\/em> koji vodi prof. dr. sc. Vlasta \u0106osovi\u0107 (PMF).<\/p>\n

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Horinzontalno laminirani – uslojeni glinoviti vapnenci Dolje formacije (Sarmat)<\/p>\n

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Model recentne sedimentacije – delta (pjeskokop Brezov Rebar)<\/p>\n

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Istra\u017eivanje prapor-paleotlo sekvence na lokalitetu\u00a0 Zmajevac (Baranja) u sklopu projekta SAPIQ<\/p>\n

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TEMELJNA GEOLO\u0160KA ISTRA\u017dIVANJA Sedimentologija, mineralogija i petrologija sedimentnih stijenaU Zavodu za geologiju provode se sedimentolo\u0161ka istra\u017eivanja koja izu\u010davaju mehanizme i uvjete talo\u017eenja klasti\u010dnih, karbonatnih, evaporitnih i silicijskih sedimentnih stijena te njihove teksturno-strukturne, petrolo\u0161ke, mineralo\u0161ke, litofacijesne, biofacijesne, kemijske, biokemijske, paleontolo\u0161ke, litostratigrafske, paleogeografske i ekolo\u0161ke karakteristike i odlike. Istra\u017eivanja se temelje na terenskim i analiti\u010dkim tehnikama (opti\u010dka […]<\/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-29040","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