{"id":37118,"date":"2020-11-30T08:20:25","date_gmt":"2020-11-30T08:20:25","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=37118"},"modified":"2020-12-18T08:27:26","modified_gmt":"2020-12-18T08:27:26","slug":"active-tectonics-in-the-kvarner-region-external-dinarides-croatia-an-alternative-approach-based-on-focused-geological-mapping-3d-seismological-and-shallow-seismic-imaging-data","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/active-tectonics-in-the-kvarner-region-external-dinarides-croatia-an-alternative-approach-based-on-focused-geological-mapping-3d-seismological-and-shallow-seismic-imaging-data\/","title":{"rendered":"Active tectonics in the Kvarner region (External Dinarides, Croatia) \u2013 an alternative approach based on focused geological mapping, 3D seismological and shallow seismic imaging data"},"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=”4.4.2″ 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_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=”4.6.6″ text_font_size=”32px” header_2_text_color=”#1e5096″]<\/p>\n

NAJNOVIJI OBJAVLJENI RADOVI<\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.4.2″][et_pb_column type=”4_4″ _builder_version=”4.4.2″][et_pb_text _builder_version=”4.7.4″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em”]<\/p>\n

Active tectonics in the Kvarner region (External Dinarides, Croatia) \u2013 an alternative approach based on focused geological mapping, 3D seismological and shallow seismic imaging data<\/h2>\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_padding=”20px||41px|||”][et_pb_row _builder_version=”4.7.4″ custom_padding=”0px|||||”][et_pb_column type=”4_4″ _builder_version=”4.7.4″][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/Frontiers_naslovnica.png” alt=”Frontiers naslovnica” title_text=”Frontiers_naslovnica” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.7.4″ width=”100%” max_width=”85%” module_alignment=”center” 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=”4.0.3″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px|||||”][et_pb_column type=”4_4″ _builder_version=”4.0.3″][et_pb_text _builder_version=”4.7.4″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true”]<\/p>\n

Rezultati dijela dosada\u0161njih multidisciplinarnih geolo\u0161kih i seizmolo\u0161kih istra\u017eivanja Kvarnera, provedenih u okviru HRZZ projekta GEOSEKVA (https:\/\/www.hgi-cgs.hr\/nacionalni-kompetativni-projekti-geosekva\/)<\/a><\/em>, objavljeni su u Open Access<\/em> \u010dasopisu Frontiers in Earth Science (https:\/\/www.frontiersin.org\/journals\/earth-science<\/a><\/em>).<\/p>\n

U znanstvenom radu Tvrtka Korbara i suradnika pod naslovom \u201eActive tectonics in the Kvarner region (External Dinarides, Croatia) \u2013 an alternative approach based on focused geological mapping, 3D seismological and shallow seismic imaging data\u201c<\/em>, objavljeni su rezultati istra\u017eivanja dijela epicentralnog podru\u010dja Rijeke, koje je poznato po umjerenoj seizmi\u010dkoj aktivnosti, ali i po povijesnim lokalno razornim potresima. Zaklju\u010deno je da na kopnu u istra\u017eivanom podru\u010dju Bakar \u2013 Krk nema jasnih manifestacija u dubini aktivnih rasjeda, koji su definirani pomo\u0107u 3D analize instrumentalno zabilje\u017eenih novijih potresa. Me\u0111utim, podatci dobiveni plitkim geoakusti\u010dnim snimanjem podmorja upu\u0107uju na postsedimentacijske deformacije kasnopleistocenskih naslaga du\u017e pojedinih zona.<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/Frontiers_web_HGI_Korbar.jpg” title_text=”Frontiers_web_HGI_Korbar” _builder_version=”4.7.4″ _module_preset=”default” width=”70%” module_alignment=”center”][\/et_pb_image][et_pb_text _builder_version=”4.7.4″ _module_preset=”default” text_font_size=”13px” max_width=”80%” module_alignment=”center”]<\/p>\n

Usporedba konceptualnih modela dana\u0161njih kasno-orogenetskih faza ekshumacije dva konvergentna borano-navla\u010dna pojasa nastala na sjeveroisto\u010dnom odnosno jugozapadnom rubu Adrije: starijeg Dinaridskog i mla\u0111eg Apeninskog.<\/p>\n

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Pretpostavlja se da su seizmolo\u0161ki definirani aktivni rasjedi uglavnom slijepi, odnosno da se tektonski pomaci du\u017e tih rasjeda u dubljim dijelovima kore vjerojatno nepravilno redistribuiraju du\u017e pripovr\u0161inskih kompleksnih tektonskih struktura formiranih tijekom ranijih faza Dinaridske orogeneze. S obzirom na zapa\u017eene lokalne deformacije kvartarnih naslaga te na povijesne, lokalno razorne potrese, a na temelju usporedbe s daleko bolje istra\u017eenim i evolucijski mla\u0111im Apeninima, zaklju\u010deno je da postoji mogu\u0107nost aktiviranja prikrivenih seizmogenih rasjeda, od kojih bi neki mogli imati i razorne posljedice. Ti rezultati upu\u0107uju na potrebu daljnjih usmjerenih istra\u017eivanja \u0161to bi trebalo doprinjeti boljoj procjeni seizmi\u010dkog hazarda u ovom relativno gusto naseljenom podru\u010dju koje je premre\u017eeno s va\u017enom nacionalnom i europskom infrastrukturom.<\/p>\n

Rad je slobodno dostupan na poveznici: <\/em>https:\/\/doi.org\/10.3389\/feart.2020.582797<\/em><\/a><\/p>\n

Intervju na Hrvatskom radiju<\/em><\/a><\/p>\n

<\/strong>Prva 3D analiza novijih potresa zabilje\u017eenih na Kvarneru – Radio Rijeka<\/em><\/a><\/p>\n

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

NAJNOVIJI OBJAVLJENI RADOVIActive tectonics in the Kvarner region (External Dinarides, Croatia) \u2013 an alternative approach based on focused geological mapping, 3D seismological and shallow seismic imaging dataRezultati dijela dosada\u0161njih multidisciplinarnih geolo\u0161kih i seizmolo\u0161kih istra\u017eivanja Kvarnera, provedenih u okviru HRZZ projekta GEOSEKVA (https:\/\/www.hgi-cgs.hr\/nacionalni-kompetativni-projekti-geosekva\/), objavljeni su u Open Access \u010dasopisu Frontiers in Earth Science (https:\/\/www.frontiersin.org\/journals\/earth-science). U znanstvenom […]<\/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-37118","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/37118","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=37118"}],"version-history":[{"count":8,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/37118\/revisions"}],"predecessor-version":[{"id":37444,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/37118\/revisions\/37444"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=37118"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}