{"id":27543,"date":"2022-02-23T15:34:04","date_gmt":"2022-02-23T14:34:04","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=27543"},"modified":"2026-01-07T14:53:27","modified_gmt":"2026-01-07T13:53:27","slug":"teams","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/research\/teams\/","title":{"rendered":"Research teams"},"content":{"rendered":"

[et_pb_section fb_built=”1″ admin_label=”2021″ _builder_version=”4.16″ _module_preset=”default” custom_padding=”27px|||||” global_colors_info=”{}”][et_pb_row column_structure=”1_3,1_3,1_3″ make_equal=”on” module_class=”slider-box slider-box-third” _builder_version=”4.16″ _module_preset=”default” width=”100%” max_width=”80%” global_colors_info=”{}”][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Active Plate Tectonic Processes<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/active-plate-tectonic-processes.jpg” title_text=”Active plate tectonic Processes” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.27.4″ global_colors_info=”{}”]<\/p>\n

Tectonic Modelling<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2026\/01\/tym-tektonicke-modelovani.jpg” title_text=”tym-tektonicke-modelovani” force_fullwidth=”on” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.27.4″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Earth Observatories<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/earth-observatories.jpg” title_text=”Earth observatories” align=”center” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_3,1_3,1_3″ make_equal=”on” module_class=”slider-box slider-box-third” _builder_version=”4.16″ _module_preset=”default” width=”100%” max_width=”80%” global_colors_info=”{}”][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Environmental\u00a0& Applied Geophysics<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/environmental-and-applied-geophysics.jpg” title_text=”Environmental and applied geophysics” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Surface Processes & Palaeoclimate<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/surface-processes-and-paleoclimate.jpg” title_text=”Surface processes and paleoclimate” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Structure of Continental Lithosphere<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/structure-of-continental-litosphere-scaled.jpg” title_text=”Structure of continental litosphere” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code admin_label=”Code” module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_3,1_3,1_3″ make_equal=”on” module_class=”slider-box slider-box-third” _builder_version=”4.16″ _module_preset=”default” width=”100%” max_width=”80%” global_colors_info=”{}”][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Seismic Wave & Source Studies<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/seismic-waves-and-source-studies-scaled.jpg” title_text=”Seismic waves and source studies” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][et_pb_text module_class=”box-slider-header” _builder_version=”4.16″ global_colors_info=”{}”]<\/p>\n

Volcanic\u00a0& Magmatic Processes<\/p>\n

[\/et_pb_text][et_pb_image src=”https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/09\/volcanic-and-magmatic-processes.jpg” title_text=”Volcanic and magmatic processes” force_fullwidth=”on” _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_image][et_pb_code module_class=”link-placeholder” _builder_version=”4.16″ global_colors_info=”{}”]<\/a>[\/et_pb_code][\/et_pb_column][et_pb_column type=”1_3″ _builder_version=”4.16″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"

Active Plate Tectonic ProcessesTectonic ModellingEarth ObservatoriesEnvironmental\u00a0& Applied GeophysicsSurface Processes & PalaeoclimateStructure of Continental LithosphereSeismic Wave & Source StudiesVolcanic\u00a0& Magmatic Processes<\/p>\n","protected":false},"author":5,"featured_media":14269,"parent":404,"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":""},"categories":[],"tags":[],"class_list":["post-27543","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"\nResearch teams - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Research teams - 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