{"id":42446,"date":"2023-09-13T09:04:53","date_gmt":"2023-09-13T09:04:53","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=42446"},"modified":"2023-09-13T09:28:04","modified_gmt":"2023-09-13T09:28:04","slug":"egu-summer-school","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/egu-summer-school\/","title":{"rendered":"EGU Summer School"},"content":{"rendered":"

[et_pb_section fb_built=”1″ _builder_version=”4.19.1″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][\/et_pb_section][et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.16″ custom_padding=”0px||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][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=”{}” theme_builder_area=”post_content”][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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/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” theme_builder_area=”post_content”][\/et_pb_slide][\/et_pb_fullwidth_slider][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.20.4″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

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

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.22.1″ text_font_size=”32px” header_2_text_color=”#1e5096″ header_2_line_height=”1.3em” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

EGU Summer School<\/strong><\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.16″ custom_padding=”20px||41px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.16″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.22.1″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”8px|||||” custom_padding=”|10px||10px|false|true” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

U periodu od 21. do 28. kolovoza 2023. godine u Ju\u017enom Tirolu (Italija) odr\u017eana je EGU ljetna \u0161kola pod nazivom \u201eStructural Analysis of Crystaline Rocks\u201c na kojoj je sudjelovao na\u0161 asistent Zavoda za Geologiju, doktorand na HRZZ projektu GOST, Matija Vukovski. Glavni organizatori i voditelji bili su Giorgio Pennacchioni (Sveu\u010dili\u0161te Padova, Italija) i Neil Mancktelow (ETH-Zurich, \u0160vicarska). \u0160kola je ugostila tridesetak doktoranada i postdoktoranada brojnih europskih sveu\u010dili\u0161ta i instituta, prvenstveno \u0161vicarskih, njema\u010dkih, francuskih, norve\u0161kih i talijanskih.<\/p>\n

Osmerodnevni program se sastojao od \u010detiri dana terenskih pokaznih vje\u017ebi i samostalnog rada te od \u010detiri dana predavanja.<\/p>\n

Terenske vje\u017ebe odr\u017eane su na visokim padinama (2600 \u2013 2800 m) u blizini jezera Neves (Lago di Neves) u Ju\u017enom Tirolu, na otvorenim, \u201epoliranim\u201c stijenama u neposrednom podno\u017eju ledenjaka Grosser M\u00f6seler. Strukturna analiza deformacijskih struktura provedena je u Varisti\u010dkom granodioritu koji pripada Tauern window-u te je u okviru Alpske orogeneze metamorfoziran u amfibolitnom facijesu, ali u domeni niskih deformacija (bez jakog Alpskog pretiska). Stoge je na terenu bilo mogu\u0107e detaljno analizirati progresivni razvoj izoliranih duktilnih smi\u010dnih zona koje su iskoristile mre\u017eu krtih prekursora (pukotina) i ranije postoje\u0107ih magmatskih ili fluidima izazvanih heterogenosti u sastavu granodiorita.<\/p>\n

Tijekom terenskih vje\u017ebi i analize polaznici su upoznati s:<\/p>\n

    \n
  • me\u0111usobnim vremenskim odnosima izme\u0111u razli\u010ditih intruzija u pre-Alpskom protolitu (primarne magmatske strukture uklju\u010duju\u0107i i one nastale putem vi\u0161e generacija intruzija kiselih i bazi\u010dnih magmi te njihovog me\u0111usobnog mije\u0161anja)<\/li>\n
  • kontrolom strukturnih i sastavnih heterogenosti na nukleaciju samostalnih i\/ili uparenih duktilnih smi\u010dnih zona (razli\u010ditim pukotinama, mineraliziranim \u017eilama, razli\u010ditim alteracijskim zonama oko \u017eila i pukotina)<\/li>\n
  • ulogom fluida u duktilnim i krtim deformacijama (kod formiranja milonita, pseudotahilita itd.)<\/li>\n
  • kinematskim odnosima razli\u010ditih deformacijskih struktura<\/li>\n
  • odnosima izme\u0111u smi\u010dnih zona koje se me\u0111usobno sijeku<\/li>\n
  • geometrijom i vezom krtih rasjeda nastalih tijekom ekshumacije.<\/li>\n<\/ul>\n

    U drugom dijelu programa u obli\u017enjem mjestu Brunico, kroz \u010detiri dana odr\u017eana je serija predavanja uz izlaganje polaznika na poster sekcijama. Predavanja su bila izlagana od strane vode\u0107ih svjetskih znanstvenika u podru\u010dju, s nekoliko europskih institucija (University of Padova, ETH-Zurich, University of Oslo, Ludwig-Maximilians University of Munich, Universit\u00e9 de Bourgogne Franche-Comt\u00e9), a pokrila su sljede\u0107e teme:<\/p>\n

      \n
    • Subsolidus duktilne deformacije pri hla\u0111enju plutona<\/li>\n
    • Fluid-stijena interakcija u rasjedima i smi\u010dnim zonama<\/li>\n
    • Deformacijski mehanizmi i lokalizacija deformacije u smi\u010dnim zonama<\/li>\n
    • Analogno i numeri\u010dko modeliranje struktura smi\u010dnih zona<\/li>\n
    • Modeliranje metodom kona\u010dnih elemenata u geoznanostima<\/li>\n
    • Dugotrajno puzanje i prijelaz u deformacije visokog naprezanja u seizmi\u010dki aktivnim smi\u010dnim zonama<\/li>\n
    • Uloga kemijskih procesa na lokalizaciju naprezanja<\/li>\n
    • Preferirana kristalografska orijentacija i njome uvjetovane fizi\u010dke karakteristike stijena<\/li>\n
    • Strukturna analiza podataka iz fotogrametrijskih modela izdanaka<\/li>\n<\/ul>\n

      [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _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\/2023\/09\/Slika-1.jpeg” title_text=”Slika 1″ align=”center” _builder_version=”4.22.1″ _module_preset=”default” width=”60%” 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_column][\/et_pb_row][et_pb_row _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.22.1″ _module_preset=”default” text_font_size=”13px” width=”67%” module_alignment=”center” custom_margin=”-29px|||||” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

      Slika 1. Voditelji i polaznici na izdancima u podno\u017eju ledenjaka Grosser M\u00f6seler.<\/em><\/em>\u00a0<\/em><\/span><\/p>\n

      [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.22.1″ _module_preset=”default” column_structure=”1_3,1_3,1_3″ theme_builder_area=”post_content”][et_pb_column _builder_version=”4.22.1″ _module_preset=”default” type=”1_3″ theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/09\/Slika-2-scaled.jpg” _builder_version=”4.22.1″ _module_preset=”default” theme_builder_area=”post_content” title_text=”Slika 2″ border_radii=”on|5px|5px|5px|5px” hover_enabled=”0″ sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.22.1″ _module_preset=”default” text_font_size=”13px” width=”67%” module_alignment=”center” custom_margin=”-29px|||||” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

      Slika 2. Jedna od brojnih diskusija o zapa\u017eenim odnosima i strukturama.<\/em>\u00a0<\/em><\/span><\/p>\n

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      Slika 3. Rezime nakon to\u010dke opa\u017eanja i samostalnog rada.<\/em>\u00a0<\/em><\/span><\/p>\n

      [\/et_pb_text][\/et_pb_column][et_pb_column _builder_version=”4.22.1″ _module_preset=”default” type=”1_3″ theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/09\/Slika-4-scaled.jpg” _builder_version=”4.22.1″ _module_preset=”default” theme_builder_area=”post_content” title_text=”Slika 4″ width=”90%” border_radii=”on|5px|5px|5px|5px” hover_enabled=”0″ sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.22.1″ _module_preset=”default” text_font_size=”13px” width=”67%” module_alignment=”center” custom_margin=”-29px|||||” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

      Slika 4. Otvoreni polirani izdanci omogu\u0107uju opa\u017eanja i najsitnijih detalja.<\/em><\/em><\/span><\/p>\n

      [\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.22.1″ _module_preset=”default” column_structure=”1_2,1_2″ theme_builder_area=”post_content”][et_pb_column _builder_version=”4.22.1″ _module_preset=”default” type=”1_2″ theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/09\/Slika-5-scaled.jpg” _builder_version=”4.22.1″ _module_preset=”default” theme_builder_area=”post_content” title_text=”Slika 5″ border_radii=”on|5px|5px|5px|5px” hover_enabled=”0″ sticky_enabled=”0″ width=”60%” module_alignment=”center”][\/et_pb_image][et_pb_text _builder_version=”4.22.1″ _module_preset=”default” text_font_size=”13px” width=”67%” module_alignment=”center” custom_margin=”-29px|||||” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

      Slika 5. Strukture mije\u0161anja bazi\u010dnih i kiselih magmi.<\/em><\/em><\/span><\/p>\n

      [\/et_pb_text][\/et_pb_column][et_pb_column _builder_version=”4.22.1″ _module_preset=”default” type=”1_2″ theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2023\/09\/Slika-6.jpeg” _builder_version=”4.22.1″ _module_preset=”default” theme_builder_area=”post_content” title_text=”Slika 6″ width=”60%” border_radii=”on|5px|5px|5px|5px” hover_enabled=”0″ sticky_enabled=”0″ module_alignment=”center”][\/et_pb_image][et_pb_text _builder_version=”4.22.1″ _module_preset=”default” text_font_size=”13px” width=”67%” module_alignment=”center” custom_margin=”-29px|||||” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

      Slika 6. Kasnono\u0107na diskusija na poster sekciji.<\/em><\/p>\n

      \u00a0<\/em><\/span><\/p>\n

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

      NOVOSTIEGU Summer SchoolU periodu od 21. do 28. kolovoza 2023. godine u Ju\u017enom Tirolu (Italija) odr\u017eana je EGU ljetna \u0161kola pod nazivom \u201eStructural Analysis of Crystaline Rocks\u201c na kojoj je sudjelovao na\u0161 asistent Zavoda za Geologiju, doktorand na HRZZ projektu GOST, Matija Vukovski. Glavni organizatori i voditelji bili su Giorgio Pennacchioni (Sveu\u010dili\u0161te Padova, Italija) i […]<\/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-42446","page","type-page","status-publish","hentry"],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/42446","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=42446"}],"version-history":[{"count":3,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/42446\/revisions"}],"predecessor-version":[{"id":42457,"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/pages\/42446\/revisions\/42457"}],"wp:attachment":[{"href":"https:\/\/www.hgi-cgs.hr\/en\/wp-json\/wp\/v2\/media?parent=42446"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}