{"id":35832,"date":"2020-10-23T12:00:52","date_gmt":"2020-10-23T12:00:52","guid":{"rendered":"http:\/\/www.hgi-cgs.hr\/?page_id=35832"},"modified":"2020-10-23T12:09:52","modified_gmt":"2020-10-23T12:09:52","slug":"studija-seizmicka-i-geoloska-mikronizacija-dijela-grada-zagreba","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/studija-seizmicka-i-geoloska-mikronizacija-dijela-grada-zagreba\/","title":{"rendered":"Studija seizmi\u010dka i geolo\u0161ka mikronizacija dijela grada Zagreba"},"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=”http:\/\/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=”http:\/\/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=”http:\/\/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=”http:\/\/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=”http:\/\/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=”http:\/\/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=”http:\/\/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

ZAVOD ZA HIDROGEOLOGIJU I IN\u017dENJERSKU GEOLOGIJU
<\/strong><\/h2>\n

Gospodarstveni (tr\u017ei\u0161ni) projekti
<\/strong><\/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=”3.25″ custom_margin=”||20px” custom_padding=”||50px”][et_pb_column type=”4_4″ _builder_version=”3.25″ custom_padding=”|||” custom_padding__hover=”|||”][et_pb_text _builder_version=”4.6.6″ text_font=”|300|||||||” ul_font=”||||||||” header_font=”||||||||” header_text_align=”center” header_2_font=”|800|||||||” header_2_text_align=”center” header_2_text_color=”#1e5096″ header_2_font_size=”54px” header_3_font=”|300|||||||” text_orientation=”center” custom_margin=”-27px||18px|||” custom_padding=”||0px|||” animation_direction=”bottom” hover_enabled=”0″ header_2_font_size_tablet=”” header_2_font_size_phone=”30px” header_2_font_size_last_edited=”on|phone” header_2_text_shadow_style=”preset1″ header_2_text_shadow_horizontal_length=”0.03em” header_2_text_shadow_vertical_length=”0.03em” header_2_text_shadow_blur_strength=”0.05em” header_2_text_shadow_color=”rgba(0,0,0,0.3)” sticky_enabled=”0″]<\/p>\n

Studija seizmi\u010dka i geolo\u0161ka mikronizacija dijela grada Zagreba
<\/strong><\/h3>\n

[\/et_pb_text][et_pb_tabs _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″][et_pb_tab title=”O projektu” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Provedeno seizmi\u010dko mikrozoniranje (2017.-2019.) rezultiralo je podjelom podsljemenske zone grada Zagreba na podru\u010dja podjednake amplifikacije tre\u0161nje tla u odnosu na osnovnu stijenu. Te zone u skladu su s normom Eurokod 8 koja sadr\u017ei upute za protupotresnu gradnju. Time je za dio podru\u010dja tj. Podsljemensku urbaniziranu zonu (podru\u010dje istra\u017eivanja ~175 km2<\/sup>) grad Zagreb dobio seizmi\u010dku podlogu neophodnu prilikom urbanisti\u010dkog planiranja, odnosno planiranja ve\u0107ih infrastrukturnih objekata, \u0161to je glavni preduvjet za dalji razvoj grada. Rezultati provedenih istra\u017eivanja (prikazanih u 4 knjige Studije, GIS projektu i karti) u svakom slu\u010daju pove\u0107avaju fond znanja i doprinose boljem poznavanju svojstava tla i stijena na podru\u010dju istra\u017eivanja, a uklopljeni su i na Kartu seizmi\u010dkog mikrozoniranja prema standardima Eurokoda 8 u M 1:25.000. Namjena karte je optimizirati planiranje i gradnju odnosno karta u ovom obliku se mo\u017ee izravno primijeniti pri planiranju razvoja istra\u017eivanog prostora u skladu sa standardima Eurokoda 8.<\/p>\n

Investitor: Grad Zagreb<\/p>\n

[\/et_pb_tab][et_pb_tab title=”Voditelj” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Glavni istra\u017eiva\u010d \/ voditelj: <\/span><\/em><\/strong>Hrvatski geolo\u0161ki institut<\/em>
<\/span><\/em><\/strong><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Suradnici” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

SVEU\u010cILI\u0160TE U ZAGREBU,<\/p>\n

PRIRODOSLOVNO MATEMATI\u010cKI FAKULTET, GEOFIZI\u010cKI ODSJEK,<\/p>\n

GEOTEHNI\u010cKI STUDIO d.o.o.,<\/p>\n

TERRA COMPACTA d.o.o<\/p>\n

[\/et_pb_tab][et_pb_tab title=”Trajanje projekta” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Datum po\u010detka i kraja projekta:<\/strong> 2017.-2019.<\/span>
<\/span><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Kategorija” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Kategorija projekta:<\/strong> <\/span>Gospodarstveni (tr\u017ei\u0161ni) projekt
<\/span><\/p>\n


<\/span><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Iznos financiranja” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Ugovoreni iznos financiranja:<\/strong>\u00a0\u00a0<\/span><\/p>\n


<\/span><\/p>\n

[\/et_pb_tab][et_pb_tab title=”Status” _builder_version=”4.6.6″ hover_enabled=”0″ sticky_enabled=”0″]<\/p>\n

Status:<\/strong> Zavr\u0161en<\/span><\/p>\n

[\/et_pb_tab][\/et_pb_tabs][et_pb_image src=”http:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/10\/Seizmicko-mikrozoniranje-prema-E8.jpg” _builder_version=”4.6.6″ _module_preset=”default” title_text=”Seizmi\u010dko mikrozoniranje prema E8″ align=”center” width=”80%” module_alignment=”center” border_radii=”on|5px|5px|5px|5px” box_shadow_style=”preset1″ box_shadow_blur=”15px” hover_enabled=”0″ sticky_enabled=”0″][\/et_pb_image][et_pb_text _builder_version=”4.6.6″ _module_preset=”default” text_font_size=”13px” hover_enabled=”0″ sticky_enabled=”0″ custom_margin=”-30px||||false|false”]<\/p>\n

Karta seizmi\u010dkog mikrozoniranj prema standardima Eurokoda 8<\/p>\n

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

ZAVOD ZA HIDROGEOLOGIJU I IN\u017dENJERSKU GEOLOGIJU Gospodarstveni (tr\u017ei\u0161ni) projekti Studija seizmi\u010dka i geolo\u0161ka mikronizacija dijela grada Zagreba Provedeno seizmi\u010dko mikrozoniranje (2017.-2019.) rezultiralo je podjelom podsljemenske zone grada Zagreba na podru\u010dja podjednake amplifikacije tre\u0161nje tla u odnosu na osnovnu stijenu. Te zone u skladu su s normom Eurokod 8 koja sadr\u017ei upute za protupotresnu gradnju. Time […]<\/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-35832","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