{"id":40901,"date":"2022-04-05T07:30:30","date_gmt":"2022-04-05T07:30:30","guid":{"rendered":"https:\/\/www.hgi-cgs.hr\/?page_id=40901"},"modified":"2022-04-05T07:37:24","modified_gmt":"2022-04-05T07:37:24","slug":"a-case-study-in-the-research-polygon-in-glina-and-dvor-municipality-croatia-landslide-susceptibility-assessment-of-geological-units","status":"publish","type":"page","link":"https:\/\/www.hgi-cgs.hr\/en\/a-case-study-in-the-research-polygon-in-glina-and-dvor-municipality-croatia-landslide-susceptibility-assessment-of-geological-units\/","title":{"rendered":"A case study in the research polygon in Glina and Dvor municipality, Croatia\u2013landslide susceptibility assessment of geological units"},"content":{"rendered":"

[et_pb_section fb_built=”1″ fullwidth=”on” _builder_version=”4.15″ custom_padding=”0px||0px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_fullwidth_slider _builder_version=”4.15″ 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=”4.15″ 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=”4.15″ 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=”4.15″ 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=”4.15″ 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=”4.15″ 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=”4.15″ 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=”4.15″ 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=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.15″ text_font_size=”32px” header_2_text_color=”#1e5096″ global_colors_info=”{}” theme_builder_area=”post_content”]<\/p>\n

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

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.15.1″ 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

A case study in the research polygon in Glina and Dvor municipality, Croatia\u2013landslide susceptibility assessment of geological units<\/h2>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=”1″ _builder_version=”4.15″ custom_padding=”20px||41px|||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_row _builder_version=”4.15″ custom_padding=”0px|||||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_image src=”https:\/\/www.hgi-cgs.hr\/wp-content\/uploads\/2020\/11\/croatica_logo.jpg” alt=”Geologia Croatica logo” title_text=”croatica_logo” align=”center” align_tablet=”center” align_phone=”” align_last_edited=”on|desktop” _builder_version=”4.15.1″ width=”25%” max_width=”35%” 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=”4.15″ min_height=”192px” custom_margin=”12px|auto||auto||” custom_padding=”0px|||||” global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_column type=”4_4″ _builder_version=”4.15″ global_colors_info=”{}” theme_builder_area=”post_content”][et_pb_text _builder_version=”4.15.1″ text_font=”||||||||” link_font=”||||||||” link_text_color=”#e09900″ custom_margin=”18px|||||” custom_padding=”|10px||10px|false|true” hover_enabled=”0″ global_colors_info=”{}” theme_builder_area=”post_content” sticky_enabled=”0″]<\/p>\n

U raduje analiziran katastar klizi\u0161ta za pilot podru\u010dje koje se nalazi na granici op\u0107ina Dvor i Glina. Katastar je izra\u0111en vizualnom interpretacijom detaljnih LiDAR podloga koje pokrivaju povr\u0161inu od pribli\u017eno 46 km2<\/sup>. Na navedenoj povr\u0161ini izdvojeno je 477 poligona klizi\u0161ta.<\/p>\n

Posebnost rada le\u017ei u analizi klizi\u0161ta nastalih u metamorfnim i magmatskim kompleksima ofiolitnog pojasa koji zauzima zna\u010dajan dio povr\u0161ine analiziranog pilot podru\u010dja.<\/p>\n

Rad je nastao zahvaljuju\u0107i podacima prikupljenim u sklopu safEarth projekta sufinanciranog od strane Interreg IPA \u2013 CBC Hrvatska \u2013 Bosna i Hercegovina \u2013 Crna Gora programa, a objavljen je u \u010dasopisu Geologia Croatica (http:\/\/www.geologia-croatica.hr\/index.php\/GC\/article\/view\/1069<\/em><\/a>).<\/p>\n

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NAJNOVIJI OBJAVLJENI RADOVIA case study in the research polygon in Glina and Dvor municipality, Croatia\u2013landslide susceptibility assessment of geological unitsU raduje analiziran katastar klizi\u0161ta za pilot podru\u010dje koje se nalazi na granici op\u0107ina Dvor i Glina. Katastar je izra\u0111en vizualnom interpretacijom detaljnih LiDAR podloga koje pokrivaju povr\u0161inu od pribli\u017eno 46 km2. Na navedenoj povr\u0161ini izdvojeno […]<\/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-40901","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