{"id":2295,"date":"2015-02-06T12:08:02","date_gmt":"2015-02-06T10:08:02","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2295"},"modified":"2015-09-01T09:32:40","modified_gmt":"2015-09-01T07:32:40","slug":"2295-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2295-2\/","title":{"rendered":""},"content":{"rendered":"<p>Geoinformatika 2013; 4(48) :\u00a043-51<\/p>\n<h4>SEISMIC WAVE PROPAGATION IN ANISOTROPIC MEDIA. INVERSE PROBLEM. II<\/h4>\n<h5><em>D.V. Malytskyy, A.Yu. Pavlova<\/em><\/h5>\n<p style=\"text-align: justify;\">A modified matrix method for solving the inverse problem for anisotropic media is developed. Atheory to determine the angles of orientation of the plane break and to build the focal mechanism of the earthquake is presented. Approbation of the matrix method is shown on real examples of events in the Transcarpathian region; a comparative analysis of synthetic seismograms with real seismic records is done.<\/p>\n<p style=\"text-align: justify;\"><strong>Keywords:<\/strong> anisotropy, tensor of seismic moment, seismic moment, focal mechanism of the earthquake, the angles of orientation of the plane break.<\/p>\n<p><em><strong><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2015\/09\/05_Malitskyi.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><\/strong><\/em><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2013; 4(48) :\u00a043-51 SEISMIC WAVE PROPAGATION IN ANISOTROPIC MEDIA. INVERSE PROBLEM. II D.V. Malytskyy, A.Yu. Pavlova A modified matrix method for solving the inverse problem for anisotropic media is developed. Atheory to determine the angles of orientation of the plane break and to build the focal mechanism of the earthquake is presented. Approbation of the matrix method is shown on real examples of events in the Transcarpathian region; a comparative analysis of synthetic seismograms with real seismic records is done. Keywords: anisotropy, tensor of seismic moment, seismic moment, focal mechanism of the earthquake, the angles of orientation of the plane break.<\/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-2295","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>- \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\/2295-2\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" 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:description\" content=\"Geoinformatika 2013; 4(48) :\u00a043-51 SEISMIC WAVE PROPAGATION IN ANISOTROPIC MEDIA. INVERSE PROBLEM. II D.V. Malytskyy, A.Yu. Pavlova A modified matrix method for solving the inverse problem for anisotropic media is developed. Atheory to determine the angles of orientation of the plane break and to build the focal mechanism of the earthquake is presented. Approbation of the matrix method is shown on real examples of events in the Transcarpathian region; a comparative analysis of synthetic seismograms with real seismic records is done. Keywords: anisotropy, tensor of seismic moment, seismic moment, focal mechanism of the earthquake, the angles of orientation of the plane break.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2295-2\/\" \/>\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=\"article:modified_time\" content=\"2015-09-01T07:32:40+00:00\" \/>\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\\\/2295-2\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2295-2\\\/\",\"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\",\"isPartOf\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/#website\"},\"primaryImageOfPage\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2295-2\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2295-2\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-02-06T10:08:02+00:00\",\"dateModified\":\"2015-09-01T07:32:40+00:00\",\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2295-2\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2295-2\\\/#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\":\"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":"- \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\/2295-2\/","og_locale":"en_US","og_type":"article","og_title":"- \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 2013; 4(48) :\u00a043-51 SEISMIC WAVE PROPAGATION IN ANISOTROPIC MEDIA. INVERSE PROBLEM. II D.V. Malytskyy, A.Yu. Pavlova A modified matrix method for solving the inverse problem for anisotropic media is developed. Atheory to determine the angles of orientation of the plane break and to build the focal mechanism of the earthquake is presented. Approbation of the matrix method is shown on real examples of events in the Transcarpathian region; a comparative analysis of synthetic seismograms with real seismic records is done. 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