{"id":21229,"date":"2021-01-19T10:45:22","date_gmt":"2021-01-19T09:45:22","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=21229"},"modified":"2026-01-21T09:35:08","modified_gmt":"2026-01-21T08:35:08","slug":"tectonic-modelling","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/","title":{"rendered":"Tectonic Modelling"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; custom_padding=&#8221;39px|||||&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_row column_structure=&#8221;3_5,2_5&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;3_5&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.27.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h4>Team Leader: Prokop Z\u00e1vada<\/h4>\n<p><strong>Our research<br \/><\/strong><\/p>\n<p>The team combines field geological mapping with scaled physical and numerical modeling of rock deformation to understand the evolution and dynamics of various geodynamic systems. We study the rock deformation mechanisms from the microscale to large-scale structures in the Earth&#8217;s&nbsp;crust. This allows us to track the evolution of geological bodies, consider the mass-transfer dynamics and make direct comparisons with geophysical models of studied areas.<\/p>\n<ul>\n<li><strong>Current projects<\/strong>\n<ul>\n<li>Ductile to brittle rheological transitions in highly crystalline lavas (project CRUSH)<\/li>\n<li>Mass transfer dynamics in the lithosphere related to folding and melting<\/li>\n<li>Structure and dynamics of shallow salt sheet intrusions (magnetotellurics, gravity and modeling) \u2013 the Tazoult salt wall in Morocco (Project GA\u010cR 24-11150S)<\/li>\n<li>Magma flow pathways in oblique rift setting of the Reykjanes peninsula (project PROVOKE)<\/li>\n<li>Magma mingling processes in mushy portions of magmatic plutons<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<p>The core facility of the team is the <a href=\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/\">Tectonic modeling laboratory.<\/a><\/p>\n<\/li>\n<\/ul>\n<p>[\/et_pb_text][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2026\/01\/20231024-140249-1024&#215;768-optimized.jpg&#8221; title_text=&#8221;20231024 140249 1024&#215;768 Optimized&#8221; _builder_version=&#8221;4.27.4&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; global_colors_info=&#8221;{}&#8221; sticky_enabled=&#8221;0&#8243;][\/et_pb_image][\/et_pb_column][et_pb_column type=&#8221;2_5&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.27.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<h4>Projects:<\/h4>\n<p>M\u0160MT (2026-2029), k\u00f3d: LUAUS26220 <a href=\"https:\/\/www.ig.cas.cz\/en\/research\/projects\/crush\/\">CatastRophical dUctile to brittle Shifts in crystal-ricH magmas (CRUSH)<\/a>, project leader Prokop Z\u00e1vada<\/p>\n<p>EXPRO: Comprehensive geophysical analysis of ongoing volcanic eruptions on the Reykjanes Peninsula \/ 2025-2030 \/<\/p>\n<p>GA\u010cR, GA24-11150S (2024 &#8211; 2026), Structure and dynamics of shallow salt sheet extrusion investigated by means of magnetotellurics, gravity and analog &amp; numerical modelling, Graham Hill, Prokop Z\u00e1vada<a href=\"https:\/\/starfos.tacr.cz\/en\/projekty\/GA24-11150S?query=3s3iaaabfzwa\"><\/a><\/p>\n<p>GA\u010cR, 22-12828S (2022-2024)\u00a0<a href=\"https:\/\/www.ig.cas.cz\/en\/research\/projects\/new-perspectives-in-magnetic-fabric-interpretation-through-3d-microstructural\/\">Perspectives in magnetic fabric interpretation through 3D analysis<\/a><\/p>\n<p>GA\u010cR, 20-18647J (2020-2022), <a href=\"https:\/\/www.ig.cas.cz\/en\/caprock-iran\/\">Influence of caprock on the growth dynamics of salt diapirs in Iran<\/a>.<\/p>\n<h4>Projects in cooperation with Centre for Lithospheric Research at Czech Geological Survey:<\/h4>\n<p>GA\u010cR, EXPRO 19-27682X (2019-2023) Principal mechanism of peripheral continental growth during supercontinent cycle.<\/p>\n<p>GA\u010cR, 19-25035S (2019-2021) Granulite-migmatite domes &#8211; insight into the Devonian and Carboniferous development of the Variscan belt.<\/p>\n<h4>Project in cooperation with Geological Institute of the CAS<\/h4>\n<p>GA\u010cR Junior, 19-02177Y (2019-2021), Magma transfer and emplacement processes in collapsing orogens<\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;4.16&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;][et_pb_text _builder_version=&#8221;4.27.4&#8243; _module_preset=&#8221;default&#8221; global_colors_info=&#8221;{}&#8221;]<\/p>\n<p><strong>People<\/strong><\/p>\n<table style=\"width: 1013px;\">\n<tbody>\n<tr>\n<td style=\"width: 146.3px; text-align: left;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21803 alignnone \" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-zavada-1.jpg\" alt=\"\" width=\"145\" height=\"145\" \/><\/td>\n<td style=\"width: 170.7px; text-align: left;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/prokop-zavada\/\">Prokop Z\u00e1vada<\/a><\/td>\n<td style=\"width: 134px; text-align: left;\">MSc, PhD<\/td>\n<td style=\"width: 237px; text-align: left;\">\n<p>Researcher<\/p>\n<p>(team leader)<\/p>\n<\/td>\n<td style=\"width: 287px; text-align: left;\">Structural geology, analogue modeling, volcanology, salt tectonics<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 146.3px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21792 alignnone size-full\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-machek.jpg\" alt=\"\" width=\"260\" height=\"260\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-machek.jpg 260w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-machek-150x150.jpg 150w\" sizes=\"(max-width: 260px) 100vw, 260px\" \/><\/td>\n<td style=\"width: 170.7px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/matej-machek\/\">Mat\u011bj Machek<\/a><\/td>\n<td style=\"width: 134px;\">MSc, PhD<\/td>\n<td style=\"width: 237px;\">Researcher<\/td>\n<td style=\"width: 287px;\">Structural geology, physical properties of rocks, analogue modeling<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 146.3px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-23545 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/04\/web2-zuzanka-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" \/><\/td>\n<td style=\"width: 170.7px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/zuzana-roxerova\/\">Zuzana Roxerov\u00e1<\/a><\/td>\n<td style=\"width: 134px;\">MSc, PhD<\/td>\n<td style=\"width: 237px;\">Researcher<\/td>\n<td style=\"width: 287px;\">Structural geology, magmatic and mountain building processes<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 146.3px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21799 alignnone \" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-stanek.jpg\" alt=\"\" width=\"144\" height=\"144\" \/><\/td>\n<td style=\"width: 170.7px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/martin-stanek\/\">Martin Stan\u011bk<\/a><\/td>\n<td style=\"width: 134px;\">MSc, PhD<\/td>\n<td style=\"width: 237px;\">Researcher<\/td>\n<td style=\"width: 287px;\">Structural geology, rock physical properties<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 146.3px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21807 alignnone size-full\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kusbach.jpg\" alt=\"\" width=\"259\" height=\"259\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kusbach.jpg 259w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kusbach-150x150.jpg 150w\" sizes=\"(max-width: 259px) 100vw, 259px\" \/><\/td>\n<td style=\"width: 170.7px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/vladimir-kusbach\/\">Vladim\u00ed\u0159 Kol\u00e1\u0159 Kusbach<\/a><\/td>\n<td style=\"width: 134px;\">MSc, PhD<\/td>\n<td style=\"width: 237px;\">Researcher<\/td>\n<td style=\"width: 287px;\">Structural geology, mountain building processes, physical properties of rocks<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 146.3px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-21805 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kryza-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" srcset=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kryza-300x300.jpg 300w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kryza-150x150.jpg 150w, https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2021\/01\/web-obr-kryza.jpg 304w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><\/td>\n<td style=\"width: 170.7px;\"><a href=\"https:\/\/www.ig.cas.cz\/en\/contact\/staff\/ondrej-kryza\/\">Ond\u0159ej Kr\u00fdza<\/a><\/td>\n<td style=\"width: 134px;\">MSc, PhD<\/td>\n<td style=\"width: 237px;\">Researcher<\/td>\n<td style=\"width: 287px;\">Structural geology, analogue modeling, mountain building processes<\/td>\n<\/tr>\n<tr>\n<td style=\"width: 146.3px;\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-35733 alignnone size-medium\" src=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2023\/09\/anna-vavrova-300x300.jpg\" alt=\"\" width=\"300\" height=\"300\" \/><\/td>\n<td style=\"width: 170.7px;\">Anna V\u00e1vrov\u00e1<\/td>\n<td style=\"width: 134px;\">\u00a0<\/td>\n<td style=\"width: 237px;\">Student<\/td>\n<td style=\"width: 287px;\">\u00a0<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><strong>\u00a0<\/strong><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=&#8221;4.16&#8243; 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We study the rock deformation mechanisms from the microscale to large-scale structures in the Earth&#8217;s&nbsp;crust. This allows us to track the evolution of [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":14285,"parent":27543,"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-21229","page","type-page","status-publish","has-post-thumbnail","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Tectonic Modelling - 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\/tectonic-modelling\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Tectonic Modelling - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"Team Leader: Prokop Z\u00e1vada Our research The team combines field geological mapping with scaled physical and numerical modeling of rock deformation to understand the evolution and dynamics of various geodynamic systems. We study the rock deformation mechanisms from the microscale to large-scale structures in the Earth&#039;s crust. This allows us to track the evolution of [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/\" \/>\n<meta property=\"og:site_name\" content=\"Dom\u016f\" \/>\n<meta property=\"article:publisher\" content=\"https:\/\/www.facebook.com\/GFUAVCR\/\" \/>\n<meta property=\"article:modified_time\" content=\"2026-01-21T08:35:08+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P32303642.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"2500\" \/>\n\t<meta property=\"og:image:height\" content=\"260\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"7 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\/\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/\",\"url\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/\",\"name\":\"Tectonic Modelling - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\",\"isPartOf\":{\"@id\":\"https:\/\/www.ig.cas.cz\/#website\"},\"primaryImageOfPage\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/#primaryimage\"},\"image\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P32303642.jpg\",\"datePublished\":\"2021-01-19T09:45:22+00:00\",\"dateModified\":\"2026-01-21T08:35:08+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/#primaryimage\",\"url\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P32303642.jpg\",\"contentUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P32303642.jpg\",\"width\":2500,\"height\":260,\"caption\":\"OLYMPUS DIGITAL CAMERA\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Dom\u016f\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Research\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/research\/\"},{\"@type\":\"ListItem\",\"position\":3,\"name\":\"Research teams\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/research\/teams\/\"},{\"@type\":\"ListItem\",\"position\":4,\"name\":\"Tectonic Modelling\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\/\/www.ig.cas.cz\/#website\",\"url\":\"https:\/\/www.ig.cas.cz\/\",\"name\":\"Dom\u016f\",\"description\":\"Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\/\/www.ig.cas.cz\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Tectonic Modelling - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/www.ig.cas.cz\/en\/research\/teams\/tectonic-modelling\/","og_locale":"en_US","og_type":"article","og_title":"Tectonic Modelling - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","og_description":"Team Leader: Prokop Z\u00e1vada Our research The team combines field geological mapping with scaled physical and numerical modeling of rock deformation to understand the evolution and dynamics of various geodynamic systems. 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