{"id":5785,"date":"2018-02-07T16:54:52","date_gmt":"2018-02-07T15:54:52","guid":{"rendered":"http:\/\/igcas.antstudio.eu\/?page_id=5785"},"modified":"2019-12-05T11:05:28","modified_gmt":"2019-12-05T10:05:28","slug":"project-ams-vs-shear-zone","status":"publish","type":"page","link":"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/","title":{"rendered":"Project AMS vs. shear zone"},"content":{"rendered":"<p>[et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;0px|0px|0px|0px&#8221; fb_built=&#8221;1&#8243; _i=&#8221;0&#8243; _address=&#8221;0&#8243;][et_pb_row column_structure=&#8221;2_3,1_3&#8243; _builder_version=&#8221;3.25&#8243; _i=&#8221;0&#8243; _address=&#8221;0.0&#8243;][et_pb_column type=&#8221;2_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; _i=&#8221;0&#8243; _address=&#8221;0.0.0&#8243; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; _i=&#8221;0&#8243; _address=&#8221;0.0.0.0&#8243;]<\/p>\n<h3><strong>AMS vs. shear zone (GJ16-25486Y)\u00a0<\/strong><\/h3>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\">Acquire new knowledge about evolution of anisotropy of magnetic susceptibility with progressive deformation. Understanding of microstructural processes controlling acquisition of magnetic fabrics. Role of inherited magnetic fabric for the formation of the AMS generated by the superpose deformation.<\/div>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\"><\/div>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\">Background and motivation<\/div>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\">Relationship between anisotropy of magnetic susceptibility (AMS) and microstructure will be studied in natural and analogue shear zones and compared with numerical modelling. Shear zones in monomineralic rocks (calcite, quartzite) are great natural laboratories for studying magnetic fabric,<\/div>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\">texture and microstructure in order to unravel the micro-scale processes controlling the AMS acquisition. Analogue models will be performed at variable tectonic settings with rheologically strain-rate dependent material. Numerical models will calculate the AMS based on real microstructure and correlate with<\/div>\n<div class=\"nova-e-text nova-e-text--size-m nova-e-text--family-sans-serif nova-e-text--spacing-s nova-e-text--color-inherit redraft-text\">observed fabrics and fabric overprints. Combined field, laboratory and numerical study should provide powerful insight in the problems of the time and space relationships between finite strain and AMS fabric. Through the assessment of the rheological behavior of matrix and embedded magnetic minerals understanding of magnetic fabric in shear zones will be enhanced, with strong applicability to general understanding of all petrofabrics.<\/div>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_3&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; _i=&#8221;1&#8243; _address=&#8221;0.0.1&#8243; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; _i=&#8221;0&#8243; _address=&#8221;0.0.1.0&#8243;]<\/p>\n<p style=\"text-align: center;\"><strong><a href=\"..\/kontakty\/seznam-pracovniku\/vladimir-kusbach\/\">Vladim\u00edr Kusbach<\/a>,<\/strong> principal investigator<\/p>\n<p style=\"text-align: center;\"><a href=\"..\/departments\/geodynamics\/\">Geodynamics<\/a><\/p>\n<p style=\"text-align: center;\"><strong><a href=\"..\/contact\/staff\/zuzana-roxerova\/\">Zuzana Roxerov\u00e1<\/a>,<\/strong> team member<\/p>\n<p style=\"text-align: center;\"><a href=\"..\/departments\/geodynamics\/\">Geodynamics<\/a><\/p>\n<p style=\"text-align: center;\"><strong><a href=\"..\/kontakty\/seznam-pracovniku\/martin-stanek\">Martin Stan\u011bk<\/a>,<\/strong>\u00a0team member<\/p>\n<p style=\"text-align: center;\"><a href=\"..\/departments\/geodynamics\/\">Geodynamics<\/a><\/p>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;56.2656px|0px|0px|0px&#8221; fb_built=&#8221;1&#8243; _i=&#8221;1&#8243; _address=&#8221;1&#8243;][et_pb_row column_structure=&#8221;1_2,1_2&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;0px|0px|28.125px|0px&#8221; _i=&#8221;0&#8243; _address=&#8221;1.0&#8243;][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; _i=&#8221;0&#8243; _address=&#8221;1.0.0&#8243; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; _i=&#8221;0&#8243; _address=&#8221;1.0.0.0&#8243;]<\/p>\n<h3><strong>Outputs<\/strong><\/h3>\n<ul>\n<li>16.-21.4. &#8211; EGU 2016 preliminary results were presented as a&nbsp;poster: Small scale shear zone in calcite: AMS and microstructure; Zuzana Roxerov\u00e1, Matej Machek, Vladim\u00edr Kusbach, Martin Racek, Pedro F. Silva.<\/li>\n<li>\n<p class=\"western\">24.-29.4. &#8211; EGU 2017 results from analysis of AMS and magnetic properties of volcanic rocks were presented as poster: Flow dynamics of dacite lava flow &#8211; AMS, microstructure and porosity case study; Prokop Z\u00e1vada, Vladim\u00edr Kusbach, Mat\u011bj Machek, Martin Stan\u011bk, and Ale\u0161 \u0160pi\u010d\u00e1k.<\/p>\n<\/li>\n<li>\n<p class=\"western\">30.4.-4.5. &#8211; DRT 2017 progress in study of natural shear zone was presented as poster: Shear zone in calcite: AMS and microstructure; V. Kusbach, Z. Roxerov\u00e1, M. Machek, M. Racek and P.&nbsp;F. Silva.<\/p>\n<\/li>\n<li>8.4.\u201313.4.&nbsp;2018 &#8211; EGU 2018 progress in study of natural shear zone was presented as talk:\u00a0Localization effect on inverse AMS fabric in marble \u2013 microstructural evidence across small-scale shear zone; Kusbach, V., Roxerov\u00e1, Z., Machek, M., Racek M., Silva, P.F.<\/li>\n<li>8.4.\u201313.4.&nbsp;2018 &#8211; EGU 2018 &#8211;\u00a0progress in study of analogue shear zone was presented as poster: Analogue modelling of magnetic fabric in ductile shear zones; Machek, M., Roxerov\u00e1, Z., Kusbach, V.<\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][et_pb_column type=&#8221;1_2&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; _i=&#8221;1&#8243; _address=&#8221;1.0.1&#8243; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; _i=&#8221;0&#8243; _address=&#8221;1.0.1.0&#8243;]<\/p>\n<h3><strong>Publications<\/strong><\/h3>\n<ul>\n<li>Kusbach, V.K., Machek, M., Roxerov\u00e1, Z.\u00a0<i>et al.<\/i><span>\u00a0Localization effect on AMS fabric revealed by microstructural evidence across small-scale shear zone in marble.\u00a0<\/span><i>Sci Rep<\/i><span>\u00a0<\/span>9<b>,<span>\u00a0<\/span><\/b><span>17483 (2019) doi:<a href=\"https:\/\/www.nature.com\/articles\/s41598-019-53794-y\">\u00a010.1038\/s41598-019-53794-y<\/a><\/span><span><span><span><strong><\/strong><\/span><\/span><\/span><\/li>\n<li>Machek, M., Z\u00e1vada, P., Roxerov\u00e1, Z., Petrovsk\u00fd, E., \u0160pi\u010d\u00e1k, A., &amp;\u00a0Kusbach, V.\u00a0(2019). Crystal mush flow in small concentrically expanded\u00a0pluton (Castle Crags pluton; Klamath Mountains, CA, USA).\u00a0<em>Geochemistry,\u00a0Geophysics, Geosystems<\/em>, 20, 1954\u2013 1974. DOI:\u00a0<a href=\"https:\/\/doi.org\/10.1029\/2018GC008018\" target=\"_blank\" rel=\"noopener noreferrer\" data-saferedirecturl=\"https:\/\/www.google.com\/url?q=https:\/\/doi.org\/10.1029\/2018GC008018&amp;source=gmail&amp;ust=1559053133556000&amp;usg=AFQjCNGlM44Mzee4qnQsBcWQi8XgcbuDsw\">10.1029\/2018GC<wbr \/>008018<\/a><\/li>\n<li><span><span>Machek, M., Kalvoda, L., Hladil, J., Roxerov\u00e1, Z., Vratislav, S.,\u00a0<span>Drahokoupil, J., Ryukhtin, V., (2018). Petrophysical record of evolution\u00a0<\/span><span>of weakly deformed low-porosity limestone revealed by small-angle\u00a0<\/span><span>neutron scattering, neutron diffraction and AMS study. <em>Geophysical\u00a0<\/em><\/span><span><em>Journal International<\/em> 215, 895-908.&nbsp;doi:<a href=\"http:\/\/dx.doi.org\/10.1093\/gji\/ggy309\">10.1093\/gji\/ggy309<\/a><\/span><\/span><\/span><\/li>\n<li><span style=\"font-size: 16px;\">Anisotropy of remanent and induced magnetization in hematite ore deformed in torsion; Mat\u011bj Machek, Eduard Petrovsk\u00fd, Zuzana Roxerov\u00e1, Vladim\u00edr Kusbach, Ramon Egli, Heinrich Siemes. Geochem. Geophys. Geosyst. (in prep.)<\/span><\/li>\n<\/ul>\n<p>[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section][et_pb_section fb_built=&#8221;1&#8243; _builder_version=&#8221;3.22&#8243; custom_padding=&#8221;0px|0px|56.2656px|0px&#8221; fb_built=&#8221;1&#8243; _i=&#8221;2&#8243; _address=&#8221;2&#8243;][et_pb_row _builder_version=&#8221;3.25&#8243; _i=&#8221;0&#8243; _address=&#8221;2.0&#8243;][et_pb_column type=&#8221;4_4&#8243; _builder_version=&#8221;3.25&#8243; custom_padding=&#8221;|||&#8221; _i=&#8221;0&#8243; _address=&#8221;2.0.0&#8243; custom_padding__hover=&#8221;|||&#8221;][et_pb_text _builder_version=&#8221;3.27.4&#8243; _i=&#8221;0&#8243; _address=&#8221;2.0.0.0&#8243;]<\/p>\n<h3 style=\"text-align: left;\"><strong>Galerie<\/strong><\/h3>\n<p>[\/et_pb_text][et_pb_gallery gallery_ids=&#8221;5499,5492,5494,5497,5496&#8243; gallery_captions=&#8221;,,,,&#8221; _builder_version=&#8221;3.0.99&#8243; _i=&#8221;1&#8243; _address=&#8221;2.0.0.1&#8243;][\/et_pb_gallery][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"<p>AMS vs. shear zone (GJ16-25486Y)\u00a0 Acquire new knowledge about evolution of anisotropy of magnetic susceptibility with progressive deformation. Understanding of microstructural processes controlling acquisition of magnetic fabrics. Role of inherited magnetic fabric for the formation of the AMS generated by the superpose deformation. Background and motivation Relationship between anisotropy of magnetic susceptibility (AMS) and microstructure [&hellip;]<\/p>\n","protected":false},"author":5,"featured_media":5566,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"<p>Vztah mezi anizotropi\u00ed magnetick\u00e9 susceptibility (AMS) a deforma\u010dn\u00ed mikrostrukturou bude studov\u00e1n v\u00a0p\u0159\u00edrodn\u00edch stri\u017en\u00fdch z\u00f3n\u00e1ch a srovn\u00e1n s analogov\u00fdm a numerick\u00fdm modelov\u00e1n\u00edm. Stri\u017en\u00e9 z\u00f3ny v\u00a0monominer\u00e1ln\u00edch hornin\u00e1ch (kalcit, kvarcit) p\u0159edstavuj\u00ed vhodn\u00e9 p\u0159\u00edrodn\u00ed laborato\u0159e ke studiu magnetick\u00e9 stavby, textury a mikrostruktury pro pochopen\u00ed mikrostrukturn\u00edch proces\u016f, kter\u00e9 kontroluj\u00ed vznik AMS.\u00a0Analogov\u00e9 modelov\u00e1n\u00ed bude prov\u00e1d\u011bno v r\u016fzn\u00fdch tektonick\u00fdch re\u017eimech pomoc\u00ed reologicky neline\u00e1rn\u00edch materi\u00e1l\u016f. Numerick\u00e9 modely budou po\u010d\u00edtat AMS na z\u00e1klad\u011b re\u00e1ln\u00e9 mikrostruktury a srovn\u00e1vat ji s\u00a0pozorovanou a m\u011b\u0159enou stavbou a stavebn\u00edmi p\u0159etisky. Kombinace ter\u00e9nn\u00ed, laboratorn\u00ed a numerick\u00e9\u00a0studie je nutn\u00e9 k pochopen\u00ed probl\u00e9mu \u010dasov\u00fdch a prostorov\u00fdch vztah\u016f mezi AMS horninovou stavbou a\u00a0kone\u010dnou deformac\u00ed. Z\u00edskan\u00e9 v\u00fdsledky p\u0159isp\u011bj\u00ed k pochopen\u00ed magnetick\u00e9 stavby ve st\u0159i\u017en\u00fdch z\u00f3n\u00e1ch na\u00a0z\u00e1klad\u011b hodnocen\u00ed vz\u00e1jemn\u00e9ho reologick\u00e9ho ovliv\u0148ov\u00e1n\u00ed z\u00e1kladn\u00ed hmoty a magnetick\u00fdch miner\u00e1l\u016f.<\/p>","_et_gb_content_width":"","footnotes":""},"categories":[],"tags":[],"class_list":["post-5785","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>Project AMS vs. shear zone - 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\/project-ams-vs-shear-zone\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Project AMS vs. shear zone - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.\" \/>\n<meta property=\"og:description\" content=\"AMS vs. shear zone (GJ16-25486Y)\u00a0 Acquire new knowledge about evolution of anisotropy of magnetic susceptibility with progressive deformation. Understanding of microstructural processes controlling acquisition of magnetic fabrics. Role of inherited magnetic fabric for the formation of the AMS generated by the superpose deformation. Background and motivation Relationship between anisotropy of magnetic susceptibility (AMS) and microstructure [&hellip;]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/\" \/>\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=\"2019-12-05T10:05:28+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P3230364-1.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=\"4 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\/project-ams-vs-shear-zone\/\",\"url\":\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/\",\"name\":\"Project AMS vs. shear zone - 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\/project-ams-vs-shear-zone\/#primaryimage\"},\"image\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/#primaryimage\"},\"thumbnailUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P3230364-1.jpg\",\"datePublished\":\"2018-02-07T15:54:52+00:00\",\"dateModified\":\"2019-12-05T10:05:28+00:00\",\"breadcrumb\":{\"@id\":\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/\"]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/#primaryimage\",\"url\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P3230364-1.jpg\",\"contentUrl\":\"https:\/\/www.ig.cas.cz\/wp-content\/uploads\/2018\/02\/P3230364-1.jpg\",\"width\":2500,\"height\":260,\"caption\":\"OLYMPUS DIGITAL CAMERA\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\/\/www.ig.cas.cz\/en\/project-ams-vs-shear-zone\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Dom\u016f\",\"item\":\"https:\/\/www.ig.cas.cz\/en\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Project AMS vs. shear zone\"}]},{\"@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":"Project AMS vs. shear zone - 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\/project-ams-vs-shear-zone\/","og_locale":"en_US","og_type":"article","og_title":"Project AMS vs. shear zone - Geofyzik\u00e1ln\u00ed \u00fastav Akademie v\u011bd \u010cR, v.v.i.","og_description":"AMS vs. shear zone (GJ16-25486Y)\u00a0 Acquire new knowledge about evolution of anisotropy of magnetic susceptibility with progressive deformation. Understanding of microstructural processes controlling acquisition of magnetic fabrics. Role of inherited magnetic fabric for the formation of the AMS generated by the superpose deformation. 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