{"id":41232,"date":"2022-06-03T10:23:29","date_gmt":"2022-06-03T10:23:29","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=41232"},"modified":"2022-06-03T11:23:21","modified_gmt":"2022-06-03T11:23:21","slug":"uzrok-petrinjskog-potresa-2020-godine-rezultati-detaljnih-analiza-potresne-serije-i-povrsinskih-manifestacija","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/uzrok-petrinjskog-potresa-2020-godine-rezultati-detaljnih-analiza-potresne-serije-i-povrsinskih-manifestacija\/","title":{"rendered":"Uzrok Petrinjskog potresa 2020. godine: Rezultati detaljnih analiza potresne serije i povr\u0161inskih manifestacija"},"content":{"rendered":"

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NOVOSTI<\/strong><\/h2>\n

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Uzrok Petrinjskog potresa 2020. godine: rezultati detaljnih analiza potresne serije i povr\u0161inskih manifestacija<\/strong><\/h2>\n

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STRU\u010cNJACI HRVATSKOG GEOLO\u0160KOG INSTITUTA U SURADNJI S ME\u0110UNARODNIM EU TIMOM SEIZMOTEKTONI\u010cARA OBJAVILI SU OPSE\u017dAN ZNANSTVENI RAD O UZROKU PETRINJSKOG POTRESA I POVR\u0160INSKIM MANIFESTACIJAMA NA \u0160IREM POTRESOM ZAHVA\u0106ENOM PODRU\u010cJU<\/strong><\/p>\n

\u00a0<\/strong>Najnoviji znanstveni rad rezultat je opse\u017enih seizmotektonskih analiza Petrinjske potresne serije i povr\u0161inskih manifestacija. U tu su svrhu stru\u010dnjaci Hrvatskog geolo\u0161kog instituta zapo\u010deli su dugotrajnu suradnju s europskim timom stru\u010dnjaka za seizmotektoniku. Europski tim sastoji se od znanstvenika iz renomiranih institucija u Francuskoj (IRSN\/PRP-ENV\/SCAN\/BERSSIN, CEREGE, LGLTPE), Italiji (INGV, Ud’A), Gr\u010dkoj (DUTH), Sloveniji (GeoZS) i Hrvatskoj (UniZG, PMF). Na \u0161irem podru\u010dju Banovine, Siska i Pokupskog izvr\u0161ena su detaljna terenska mjerenja te snimanja daljinskim metodama koseizmi\u010dkih i posteizmi\u010dkih pojava kao \u0161to su\u00a0 pukotine na cesti, u tlu i u stijeni, boranje povr\u0161inskih dijelova tla (eng. mole tracks<\/em>), deformacije gra\u0111evinskih objekata i infrastrukture, likvefakcije, odroni i klizi\u0161ta. Za \u0161ire podru\u010dje Hrastovi\u010dke gore izra\u0111en je digitalni model reljefa visoke rezolucije na temelju podataka zra\u010dnog laserskog skeniranja (LiDAR). Tijekom prolje\u0107a i ljeta 2020. godine na terenu su analizirani podaci geomorfolo\u0161kih markera koji upu\u0107uju na dugotrajnu tektonsku aktivnost tzv. Petrinjsko-Pokupske rasjedne zone. Temeljem Sentinel-1 podataka satelitske radarske inteferometrije\u00a0 izra\u0111eni su prikazi koji su kori\u0161teni za procjenu obuhvata i veli\u010dine povr\u0161inskih deformacija. GNSS opa\u017eanjem trajno stabiliziranih geodetskih to\u010daka u zoni deformacije dobiveni su apsolutni pomaci povr\u0161ine terena. Duboki refleksijski seizmi\u010dki profili i bu\u0161otinski podaci kori\u0161teni su za odre\u0111ivanje podpovr\u0161inskog strukturno-stratigrafskog sklopa. \u00a0\u00a0\u00a0\u00a0<\/p>\n

Potresna serija vezana uz glavni petrinjski potres 2020. godine, momentne magnitude (Mw) 6.4, dogodila se na procijenjenoj dubini u rasponu od 8 \u2013 13 km (prema podacima 6 institucija), du\u017e desnog pru\u017enog rasjeda Petrinjsko-Pokupske rasjedne zone. Konvergencija Europske i Jadranske mikroplo\u010de vjerojatni je uzrok reaktivacije struktura u podru\u010dju Savske suturne zone te pojave transpresijskih deformacija vidljivih i na povr\u0161ini. Strukturno-tektonske deformacije uzrokovale su nastanak pozitivne cvjetne strukture, na povr\u0161ini vidljive kao Hrastovi\u010dka gora. Navedeni procesi pod povr\u0161inom uzrokovali su nastanak koseizmi\u010dkih i postseizmi\u010dkih pojava na povr\u0161ini, u vidu pukotina u tlu i stijenama. To\u010dnije, pomaci u dubini u zoni aktivnog rasjeda uzrokovali su pojavu e\u0161aloniranih povr\u0161inskih rasjeda, du\u017e zone duljine 13 km, orijentacije SZ \u2013 JI. Mjerenja navedenih pojava na podru\u010dju Hrastovi\u010dke gore ukazuju na desni tip pomaka, prosje\u010dnog iznosa od 10 cm, dok maksimalne vrijednosti pomaka iznose do 38 cm. Na osnovi mjerenih GPS to\u010daka mjerenja prije i poslije potresa, ustanovljen je maksimalni pomak povr\u0161ine terena od 75 cm u smjeru istok \u2013 jugoistok. Primjerice, u gradu Sisku povr\u0161ina terena se pomaknula za oko 7 cm u smjeru istoka, u gradu Glini za oko 6 cm u smjeru SZ, dok je u zoni epicentra (selo Stra\u0161nik) zabilje\u017een pomak od 65 cm u smjeru SZ. Mjereni kumulativni pomak dugotrajne tektonske aktivnosti du\u017e rasjedne zone iznosi do 560 m, tijekom posljednjih 7 do 2.8 mil. god. Prema tome, srednji procijenjeni godi\u0161nji pomak iznosi izme\u0111u 0.3 mm i 0.6 mm.\u00a0 \u00a0<\/p>\n

Gibanje potresnih valova kroz vodom saturirane i rastresite sedimente uzrokovalo je pojavu likvefakcije, na podru\u010dju udaljenom \u010dak i do 20 km od zone epicentra potresa. Ove pojave zabilje\u017eene su najju\u017enije kod grada Gline pa sve do podru\u010dja sjeverno od grada Siska. Navedene pojave detaljno su analizirane temeljem satelitskih i snimaka zabilje\u017eenih bespilotnim zrakoplovnim sustavom te mjerenjima geometrije pukotina i tipa likvefakcija na terenu. Zaklju\u010duje se da je geometrija likvefakcija u skladu s geometrijom i stratigrafskom heterogeno\u0161\u0107u fluvijalnih sedimenata plio-kvartarne starosti i recentnih sedimenata u dolinama rijeke Kupe, Gline, Maje, Utinje i Save. Likvefakcije se javljaju u zonama prijelaza poplavne ravnice u paleokanal, uz recentne rije\u010dne nasipe, unutar napu\u0161tenih (paleo)meandara i sli\u010dno. Fizikalni uzrok likvefakcija je kombinacija tenzijskih sila i smicanja tijekom refrakcije potresnih valova, uzrokovanih mehani\u010dkim kontrastom unutar sedimenata. Drugim rije\u010dima, javljaju se u zonama maksimalne deformacije povr\u0161ine (temeljem interpretacije InSAR mjerenja) i prate trend (paleo) rije\u010dnih sustava. Na \u0161irem podru\u010dju zabilje\u017eeni su odroni i klizanja na povr\u0161ini terena. Navedene pojave ve\u0107inom su povezane s koseizmi\u010dkom reaktivacijom postoje\u0107ih sustava u stijenama (npr. pukotine u kalkarenitima badenske starosti) ili plohama klizanja u vodom natopljenim neo\u010dvrsnutim sedimentima plio-kvartarne starosti na padinama. \u00a0<\/p>\n

Istra\u017eivanja su nastavljena tijekom 2021. i 2022. godine. Na osnovi provedenih geofizi\u010dkih snimanja profila metodom elektri\u010dne tomografije i georadarom odre\u0111ene su potencijalne lokacije za paleoseizmolo\u0161ka istra\u017eivanja. Tako su stru\u010dnjaci s HGI-a u suradnji s EU timom tijekom travnja ove godine otvorili prvi paleoseizmolo\u0161ki rov u Republici Hrvatskoj, a u planu ih je jo\u0161 nekoliko. Vjerujemo da \u0107e nastavak paleoseizmolo\u0161kih istra\u017eivanja na podru\u010dju Petrinje i okolice donijeti vrijedna saznanja o mehanizmima Petrinjsko-Pokupskog rasjeda te u budu\u0107nosti omogu\u0107iti bolju procjenu njegovog seizmi\u010dkog potencijala.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_3,1_3,1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-1.png” alt=”Polo\u017eaj, geometrija rasjedne zone i \u0161iri strukturni sklop petrinjskog i sisa\u010dkog podru\u010dja” title_text=”slika 1″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-1.png” _builder_version=”4.17.4″ _module_preset=”default” width=”95%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Polo\u017eaj, geometrija rasjedne zone i \u0161iri strukturni sklop petrinjskog i sisa\u010dkog podru\u010dja<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-4.png” alt=”InSAR analize povr\u0161inskih deformacija u usporedbi s prikazanom trasom kartiranih koseizmi\u010dkih povr\u0161inskih pukotina.” title_text=”slika 4″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-4.png” _builder_version=”4.17.4″ _module_preset=”default” width=”95%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

InSAR analize povr\u0161inskih deformacija u usporedbi s prikazanom trasom kartiranih koseizmi\u010dkih povr\u0161inskih pukotina.<\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-2.png” alt=”Prostorna distribucija epicentara potresne serije.” title_text=”slika 2″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-2.png” align=”center” _builder_version=”4.17.4″ _module_preset=”default” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” width=”77%” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||65px||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Prostorna distribucija epicentara potresne serije.<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-5.png” alt=”Apsolutni pomaci geodetskih to\u010daka u usporedbi s prikazanom trasom kartiranih koseizmi\u010dkih povr\u0161inskih pukotina.” title_text=”slika 5″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-5.png” _builder_version=”4.17.4″ _module_preset=”default” width=”71%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Apsolutni pomaci geodetskih to\u010daka u usporedbi s prikazanom trasom kartiranih koseizmi\u010dkih povr\u0161inskih pukotina.<\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-3.png” alt=”Prostorna distribucija hipocentara potresne serije.” title_text=”slika 3″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/sl3.png” align=”center” _builder_version=”4.17.4″ _module_preset=”default” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” width=”80%” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||64px||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Prostorna distribucija hipocentara potresne serije.<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-6.png” alt=”20 m duga koseizmi\u010dka povr\u0161inska pukotina koja predstavlja odraz rasjeda na podru\u010dju aluvijalne lepeze jugozapadno od sela Kri\u017e Hrastova\u010dki.” title_text=”slika 6″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-6.png” _builder_version=”4.17.4″ _module_preset=”default” width=”100%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” custom_margin=”50px||||false|false” custom_padding=”50px||||false|false” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

20 m duga koseizmi\u010dka povr\u0161inska pukotina koja predstavlja odraz rasjeda na podru\u010dju aluvijalne lepeze jugozapadno od sela Kri\u017e Hrastova\u010dki.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_2,1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-7.png” alt=”Povr\u0161inska pukotina koja predstavlja direktan odraz rasjeda na povr\u0161ini u podru\u010dju sela \u017dupi\u0107. ” title_text=”slika 7″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-7.png” _builder_version=”4.17.4″ _module_preset=”default” width=”65%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″ align=”right”][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Povr\u0161inska pukotina koja predstavlja direktan odraz rasjeda na povr\u0161ini u podru\u010dju sela \u017dupi\u0107.<\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-8.png” alt=”Dugotrajni tektonski pomaci rekonstruirani geomorfolo\u0161kom analizom LIDAR snimaka reljefa.” title_text=”slika 8″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-8.png” align=”center” _builder_version=”4.17.4″ _module_preset=”default” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” width=”94%” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Dugotrajni tektonski pomaci rekonstruirani geomorfolo\u0161kom analizom LIDAR snimaka reljefa.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_2,1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-9.png” alt=”Pojave likvefakcija s prate\u0107im izba\u010denim pijeskom i bo\u010dnim \u0161irenjem. ” title_text=”slika 9″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-9.png” _builder_version=”4.17.4″ _module_preset=”default” width=”75%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″ align=”right”][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Pojave likvefakcija s prate\u0107im izba\u010denim pijeskom i bo\u010dnim \u0161irenjem.<\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-10.png” alt=”Pojave likvefakcija koje su kartirane kabinetski, a zatim provjerene i izmjerene na terenu. Pojave su vezane uz fluvijalne rije\u010dne sustave Kupe, Save i Gline.” title_text=”slika 10″ url=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-10.png” align=”center” _builder_version=”4.17.4″ _module_preset=”default” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” width=”70%” sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

Pojave likvefakcija koje su kartirane kabinetski, a zatim provjerene i izmjerene na terenu. Pojave su vezane uz fluvijalne rije\u010dne sustave Kupe, Save i Gline.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_2,1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-11.png” alt=”Pojave likvefakcija s prate\u0107im izba\u010denim pijeskom i bo\u010dnim \u0161irenjem. ” title_text=”slika 11″ _builder_version=”4.17.4″ _module_preset=”default” width=”80%” module_alignment=”center” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″ align=”center” custom_padding=”|||100px|false|false” custom_margin=”||||false|false”][\/et_pb_image][\/et_pb_column][et_pb_column type=”1_2″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-12.jpg” alt=”Pojave likvefakcija koje su kartirane kabinetski, a zatim provjerene i izmjerene na terenu. Pojave su vezane uz fluvijalne rije\u010dne sustave Kupe, Save i Gline.” title_text=”slika 12″ align=”center” _builder_version=”4.17.4″ _module_preset=”default” hover_enabled=”0″ border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” global_colors_info=”{}” theme_builder_area=”post_content” width=”38%” sticky_enabled=”0″ custom_margin=”|||-100px|false|false”][\/et_pb_image][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.17.4″ _module_preset=”default” theme_builder_area=”post_content”][et_pb_column _builder_version=”4.17.4″ _module_preset=”default” type=”4_4″ theme_builder_area=”post_content”][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″ custom_padding=”|250px||0px|false|false”]<\/p>\n

Paleoseizmolo\u0161ki rov u Hrastovici, travanj 2022.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.17.4″ _module_preset=”default” theme_builder_area=”post_content”][et_pb_column _builder_version=”4.17.4″ _module_preset=”default” type=”4_4″ theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2022\/06\/slika-13.png” _builder_version=”4.17.4″ _module_preset=”default” theme_builder_area=”post_content” title_text=”slika 13″ width=”50%” box_shadow_style=”preset1″ box_shadow_blur=”15px” border_radii=”on|5px|5px|5px|5px” hover_enabled=”0″ sticky_enabled=”0″ custom_margin=”|||150px|false|false”][\/et_pb_image][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” text_font_size=”13px” custom_margin=”-30px||||false|false” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″ custom_padding=”|250px||0px|false|false”]<\/p>\n

Bo\u010dno \u0161irenje u blizini Male Gorice, lijeva obala rijeke Kupe, travanj 2022.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.17.4″ _module_preset=”default” theme_builder_area=”post_content”][et_pb_column _builder_version=”4.17.4″ _module_preset=”default” type=”4_4″ theme_builder_area=”post_content”][et_pb_text _builder_version=”4.17.4″ _module_preset=”default” theme_builder_area=”post_content” hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Referenca<\/strong>:<\/p>\n

Baize, S., Amoroso, S., Beli\u0107, N., Benedetti, L., Boncio, P., Budi\u0107, M., Cinti, F. R., Henriquet, M., Jam\u0161ek Rupnik, P., Kordi\u0107, B., Marku\u0161i\u0107, S., Minarelli, L., Pantosti, D., Pucci, S., \u0160peli\u0107, M., Testa, A., Valkaniotis, S., Vukovski, M., Atanackov, J., Barba\u010da, J., Bavec, M., Brajkovi\u010d, R., Br\u010di\u0107, V., Caciagli, M., Celarc, B., Civico, R., De Martini, P. M., Filjak, R., Iezzi, F., Moulin, A., Kure\u010di\u0107, T., M\u00e9tois, M., Nappi, R., Novak, A., Novak, M., Pace, B., Palenik, D., Ricci, T. (2022): Environmental effects and seismogenic source characterization of the December 2020 earthquake sequence near Petrinja, Croatia \u2013 Geophysical Journal International\u00a0\u00a0 <\/span> (https:\/\/doi.org\/10.1093\/gji\/ggac123<\/em><\/a>)<\/p>\n

Autori teksta<\/strong>: Marko \u0160peli\u0107, Matija Vukovski, Nikola Beli\u0107, Marko Budi\u0107 i Branko Kordi\u0107 (Zavod za Geologiju, Hrvatski geolo\u0161ki institut)<\/p>\n

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

NOVOSTIUzrok Petrinjskog potresa 2020. godine: rezultati detaljnih analiza potresne serije i povr\u0161inskih manifestacijaSTRU\u010cNJACI HRVATSKOG GEOLO\u0160KOG INSTITUTA U SURADNJI S ME\u0110UNARODNIM EU TIMOM SEIZMOTEKTONI\u010cARA OBJAVILI SU OPSE\u017dAN ZNANSTVENI RAD O UZROKU PETRINJSKOG POTRESA I POVR\u0160INSKIM MANIFESTACIJAMA NA \u0160IREM POTRESOM ZAHVA\u0106ENOM PODRU\u010cJU \u00a0Najnoviji znanstveni rad rezultat je opse\u017enih seizmotektonskih analiza Petrinjske potresne serije i povr\u0161inskih manifestacija. U […]<\/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-41232","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/41232","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=41232"}],"version-history":[{"count":4,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/41232\/revisions"}],"predecessor-version":[{"id":41252,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/41232\/revisions\/41252"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=41232"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}