{"id":3269,"date":"2015-03-25T13:52:33","date_gmt":"2015-03-25T11:52:33","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3269"},"modified":"2015-03-25T13:52:33","modified_gmt":"2015-03-25T11:52:33","slug":"2009-3-68-73","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2009-3-68-73\/","title":{"rendered":"2009; 3 : 68-73"},"content":{"rendered":"<p>Geoinformatika 2009; 3 :\u00a068-73<\/p>\n<h4>MATHEMATICAL DESIGN OF TECTONOFACES OF METAMORPHIC ROCKS IN KRIVBAS EPIZONE<\/h4>\n<h5><em>Prodayvoda G.T., Vyzhva S.A., Bezrodniy D.A., Bezrodna I.M.<\/em><\/h5>\n<p style=\"text-align: justify;\">Influence of fragile deformations on the acoustic and elastic parameters of anisotropy is considered on the models of \u201cbiotitic quartzite\u201d, which are characterized by different systems of orientation of mikrocracks and minerals, and on the model of the combined systems of \u201cferrous quartzite\u201d. It is set that, with the growth of the level of deformation transformations in conditions of epizone, parameters of anisotropy change, in particular, the parameters of integral and differential coefficients of acoustic and clastic anisotropy grow, but in a different measure. \u0422his can serve as a reliable indicator while determining the mark of tectonic facies.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/Prodajvoda.pdf\"><img loading=\"lazy\" decoding=\"async\" class=\"wp-image-790 alignleft\" src=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" alt=\"pdf\" width=\"48\" height=\"48\" srcset=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg 128w, http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf-150x150.jpg 150w\" sizes=\"auto, (max-width: 48px) 100vw, 48px\" \/><\/a><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2009; 3 :\u00a068-73 MATHEMATICAL DESIGN OF TECTONOFACES OF METAMORPHIC ROCKS IN KRIVBAS EPIZONE Prodayvoda G.T., Vyzhva S.A., Bezrodniy D.A., Bezrodna I.M. Influence of fragile deformations on the acoustic and elastic parameters of anisotropy is considered on the models of \u201cbiotitic quartzite\u201d, which are characterized by different systems of orientation of mikrocracks and minerals, and on the model of the combined systems of \u201cferrous quartzite\u201d. It is set that, with the growth of the level of deformation transformations in conditions of epizone, parameters of anisotropy change, in particular, the parameters of integral and differential coefficients of acoustic and clastic anisotropy grow, but in a different measure. \u0422his can serve as a reliable indicator while determining the mark of tectonic facies.<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"open","ping_status":"open","template":"","meta":{"footnotes":""},"class_list":["post-3269","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.6 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>2009; 3 : 68-73 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"http:\/\/www.geology.com.ua\/en\/2009-3-68-73\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2009; 3 : 68-73 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"og:description\" content=\"Geoinformatika 2009; 3 :\u00a068-73 MATHEMATICAL DESIGN OF TECTONOFACES OF METAMORPHIC ROCKS IN KRIVBAS EPIZONE Prodayvoda G.T., Vyzhva S.A., Bezrodniy D.A., Bezrodna I.M. Influence of fragile deformations on the acoustic and elastic parameters of anisotropy is considered on the models of \u201cbiotitic quartzite\u201d, which are characterized by different systems of orientation of mikrocracks and minerals, and on the model of the combined systems of \u201cferrous quartzite\u201d. It is set that, with the growth of the level of deformation transformations in conditions of epizone, parameters of anisotropy change, in particular, the parameters of integral and differential coefficients of acoustic and clastic anisotropy grow, but in a different measure. \u0422his can serve as a reliable indicator while determining the mark of tectonic facies.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2009-3-68-73\/\" \/>\n<meta property=\"og:site_name\" content=\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\" \/>\n<meta property=\"og:image\" content=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"1 minute\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/\",\"name\":\"2009; 3 : 68-73 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-25T11:52:33+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/#primaryimage\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"contentUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\"},{\"@type\":\"BreadcrumbList\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2009-3-68-73\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"2009; 3 : 68-73\"}]},{\"@type\":\"WebSite\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\",\"name\":\"\u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb\",\"description\":\"\u0426\u0435\u043d\u0442\u0440 \u043c\u0435\u043d\u0435\u0434\u0436\u043c\u0435\u043d\u0442\u0443 \u0442\u0430 \u043c\u0430\u0440\u043a\u0435\u0442\u0438\u043d\u0433\u0443 \u0432 \u0433\u0430\u043b\u0443\u0437\u0456 \u043d\u0430\u0443\u043a \u043f\u0440\u043e \u0417\u0435\u043c\u043b\u044e\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/?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":"2009; 3 : 68-73 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","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":"http:\/\/www.geology.com.ua\/en\/2009-3-68-73\/","og_locale":"en_US","og_type":"article","og_title":"2009; 3 : 68-73 - \u0421\u0430\u0439\u0442 \u0436\u0443\u0440\u043d\u0430\u043b\u0443 \u00ab\u0413\u0435\u043e\u0456\u043d\u0444\u043e\u0440\u043c\u0430\u0442\u0438\u043a\u0430\u00bb","og_description":"Geoinformatika 2009; 3 :\u00a068-73 MATHEMATICAL DESIGN OF TECTONOFACES OF METAMORPHIC ROCKS IN KRIVBAS EPIZONE Prodayvoda G.T., Vyzhva S.A., Bezrodniy D.A., Bezrodna I.M. Influence of fragile deformations on the acoustic and elastic parameters of anisotropy is considered on the models of \u201cbiotitic quartzite\u201d, which are characterized by different systems of orientation of mikrocracks and minerals, and on the model of the combined systems of \u201cferrous quartzite\u201d. 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