{"id":27230,"date":"2022-01-22T21:27:12","date_gmt":"2022-01-22T20:27:12","guid":{"rendered":"https:\/\/www.ig.cas.cz\/?page_id=27230"},"modified":"2023-08-21T12:11:22","modified_gmt":"2023-08-21T10:11:22","slug":"shear-zones","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/","title":{"rendered":"Development of fabrics in experimental shear zones"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; admin_label=&#8221;section&#8221; _builder_version=&#8221;3.22&#8243;][et_pb_row column_structure=&#8221;3_4,1_4&#8243; admin_label=&#8221;row&#8221; _builder_version=&#8221;3.25&#8243; background_size=&#8221;initial&#8221; background_position=&#8221;top_left&#8221; background_repeat=&#8221;repeat&#8221;][et_pb_column type=&#8221;3_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<p>PROJECT DESCRIPTION<\/p>\n<p>The anisotropy of magnetic susceptibility (AMS) reflects the overall microstructural configuration and particular microstructural components of rocks (Machek et al., 2018). In this study, we try to identify what are the micro-scale processes that control the development of AMS during the formation of tectonic shear zones (e.g. deformation gradient and localization) and describe the relationship between AMS and applied strain. The apparatus for analogue modelling is designed as a&nbsp;large sandbox with variable width of the central zone of shearing (Kusbach et al., 2019). The movement of the box is provided by a&nbsp;stepper motor and the deformation rate can be adjusted by a&nbsp;gearbox. The experiments are created using colored plaster of Paris. Homogeneously admixed fine-grained magnetite is used to trace the material flow by measuring AMS fabrics. The final solidified model is cut in a&nbsp;regular grid, processed by image analysis and drilled in a&nbsp;3D mesh of 1 cm wide samples, which are analyzed in terms of AMS. The used material displays a&nbsp;shear thinning thixotropic rheology and is capable of reproducing the strain localization in natural rocks.<\/p>\n<p>[\/et_pb_text][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/03\/shearzone_nature.jpg&#8221; title_text=&#8221;ShearZone Nature&#8221; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221; width=&#8221;80%&#8221; max_width=&#8221;80%&#8221;][\/et_pb_image][et_pb_text _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221; min_height=&#8221;83.2px&#8221;]<\/p>\n<p><em><i>Low-temperature shear zone within marble rocks in Portugal subjected to detailed study. The colored circles represent oriented drill holes (see\u00a0 Kusbach et al., 2019 for detailed information).<\/i><br \/><\/em><\/p>\n<p>[\/et_pb_text][et_pb_image src=&#8221;https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/01\/vlada_results.jpg&#8221; title_text=&#8221;Vlada Results&#8221; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221; width=&#8221;80%&#8221; max_width=&#8221;80%&#8221;][\/et_pb_image][et_pb_text _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;]<\/p>\n<p><em><i>Results of simple shear experiments using sheared and solidified plaster. (a) Experimental shear apparatus. (b) Overview of the model setup. (c) shows a&nbsp;plan view photograph of the experimental shear zone and (d) displays the patch of the drilled cores in detail. (e) An example of magnetic anisotropy data in the form of T parameter (related to shape of AMS ellipsoid).<\/i><\/em><\/p>\n<p>[\/et_pb_text][et_pb_toggle title=&#8221;Publications&#8221; admin_label=&#8221;Toggle&#8221; _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221;]<\/p>\n<ul>\n<li>Kusbach, V. K., Machek, M., Roxerov\u00e1, Z., Racek, M., &amp; Silva, P.&nbsp;F., 2019. Localization effect on AMS fabric revealed by microstructural evidence across small-scale shear zone in marble. Sci Rep 9, 17483, doi:<a href=\"https:\/\/www.nature.com\/articles\/s41598-019-53794-y\"> 10.1038\/s41598-019-53794-y<\/a><\/li>\n<li>Machek, M., Z\u00e1vada, P., Roxerov\u00e1, Z., Petrovsk\u00fd, E., \u0160pi\u010d\u00e1k, A., &amp; Kusbach, V., 2019. Crystal mush flow in small concentrically expanded pluton (Castle Crags pluton; Klamath Mountains, CA, USA). Geochemistry, Geophysics, Geosystems, 20, 1954\u2013 1974, doi:<a href=\"https:\/\/doi.org\/10.1029\/2018GC008018\"> 10.1029\/2018GC008018<\/a><\/li>\n<\/ul>\n<p>[\/et_pb_toggle][\/et_pb_column][et_pb_column type=&#8221;1_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;4.6.0&#8243; _module_preset=&#8221;default&#8221; hover_enabled=&#8221;0&#8243; sticky_enabled=&#8221;0&#8243;]<\/p>\n<h4><strong>Period<\/strong><\/h4>\n<p>2016-2019<\/p>\n<p>&nbsp;<\/p>\n<h4><strong>Researcher<\/strong><\/h4>\n<p>Zuzana Roxerov\u00e1<\/p>\n<p>Vladim\u00edr Kusbach<\/p>\n<p>Mat\u011bj Machek<\/p>\n<p>&nbsp;<\/p>\n<p>&nbsp;<\/p>\n<h4><strong>Funding<\/strong><\/h4>\n<ul>\n<li>GA\u010cR (No. GJ16-25486Y)<\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>PROJECT DESCRIPTION The anisotropy of magnetic susceptibility (AMS) reflects the overall microstructural configuration and particular microstructural components of rocks (Machek et al., 2018). In this study, we try to identify what are the micro-scale processes that control the development of AMS during the formation of tectonic shear zones (e.g. deformation gradient and localization) and describe [&hellip;]<\/p>\n","protected":false},"author":28,"featured_media":27255,"parent":26857,"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":[126],"class_list":["post-27230","page","type-page","status-publish","has-post-thumbnail","hentry","tag-projects-grants"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.9 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Development of fabrics in experimental shear zones - 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\/observatories\/tect-mod-lab\/shear-zones\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Development of fabrics in experimental shear zones - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"PROJECT DESCRIPTION The anisotropy of magnetic susceptibility (AMS) reflects the overall microstructural configuration and particular microstructural components of rocks (Machek et al., 2018). In this study, we try to identify what are the micro-scale processes that control the development of AMS during the formation of tectonic shear zones (e.g. deformation gradient and localization) and describe [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/\" \/>\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=\"2023-08-21T10:11:22+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/01\/backgroundimage-12-scaled.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"2880\" \/>\n\t<meta property=\"og:image:height\" content=\"315\" \/>\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=\"3 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\/observatories\/tect-mod-lab\/shear-zones\/\",\"url\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/\",\"name\":\"Development of fabrics in experimental shear zones - 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\/observatories\/tect-mod-lab\/shear-zones\/#primaryimage\"},\"image\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/01\/backgroundimage-12-scaled.jpg\",\"datePublished\":\"2022-01-22T20:27:12+00:00\",\"dateModified\":\"2023-08-21T10:11:22+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/#primaryimage\",\"url\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/01\/backgroundimage-12-scaled.jpg\",\"contentUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2022\/01\/backgroundimage-12-scaled.jpg\",\"width\":2880,\"height\":315},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/shear-zones\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Dom\u016f\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Observatories\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/\"},{\"@type\":\"ListItem\",\"position\":3,\"name\":\"Tectonic modelling laboratory\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/observatories\/tect-mod-lab\/\"},{\"@type\":\"ListItem\",\"position\":4,\"name\":\"Development of fabrics in experimental shear zones\"}]},{\"@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":"Development of fabrics in experimental shear zones - 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\/observatories\/tect-mod-lab\/shear-zones\/","og_locale":"en_US","og_type":"article","og_title":"Development of fabrics in experimental shear zones - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","og_description":"PROJECT DESCRIPTION The anisotropy of magnetic susceptibility (AMS) reflects the overall microstructural configuration and particular microstructural components of rocks (Machek et al., 2018). 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