{"id":2881,"date":"2015-03-10T10:07:56","date_gmt":"2015-03-10T08:07:56","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2881"},"modified":"2015-04-09T13:05:06","modified_gmt":"2015-04-09T11:05:06","slug":"2011-1-51-57","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2011-1-51-57\/","title":{"rendered":"2011; 1 : 51-57"},"content":{"rendered":"<p>Geoinformatika 2011; 1 :\u00a051-56<\/p>\n<h4>MODELING OF DEFLECTED MODE AND ANOMALOUS GRAVITY FIELD AROUND EARTHQUAKE CENTRE<\/h4>\n<h5><em>Lubkov M.V.<\/em><\/h5>\n<p style=\"text-align: justify;\">Stress-deformable state and anomalous gravity field in the earthquake centre with displacement along fault spread were modeled on the base of variation finite element method elaborated for elastic foliated shells. It was shown that in the case of monolithic rocks shift displacements, stresses and anomalous gravity field distributions around earthquake centre had a universal character. Those are not dependent on the thickness of elastic lithosphere, on the geological composition and linear dimensions of the earthquake centre. At the same time fracturing of geological rocks leads to the qualitative changes on the distribution patterns. Some irregular maximum and minimum zones can be seen. Their number grows as the rock fracturing increases.<\/p>\n<p><strong>Keywords:<\/strong> earthquake centre, mode of deformation, gravity field.<\/p>\n<p style=\"text-align: justify;\"><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/07_Lubkov.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>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2011; 1 :\u00a051-56 MODELING OF DEFLECTED MODE AND ANOMALOUS GRAVITY FIELD AROUND EARTHQUAKE CENTRE Lubkov M.V. Stress-deformable state and anomalous gravity field in the earthquake centre with displacement along fault spread were modeled on the base of variation finite element method elaborated for elastic foliated shells. It was shown that in the case of monolithic rocks shift displacements, stresses and anomalous gravity field distributions around earthquake centre had a universal character. Those are not dependent on the thickness of elastic lithosphere, on the geological composition and linear dimensions of the earthquake centre. At the same time fracturing of geological rocks leads to the qualitative changes on the distribution patterns. Some irregular maximum and minimum zones can be seen. Their number grows as the rock fracturing increases. Keywords: earthquake centre, mode of deformation, gravity field.<\/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-2881","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>2011; 1 : 51-57 - \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\/2011-1-51-57\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2011; 1 : 51-57 - \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 2011; 1 :\u00a051-56 MODELING OF DEFLECTED MODE AND ANOMALOUS GRAVITY FIELD AROUND EARTHQUAKE CENTRE Lubkov M.V. Stress-deformable state and anomalous gravity field in the earthquake centre with displacement along fault spread were modeled on the base of variation finite element method elaborated for elastic foliated shells. It was shown that in the case of monolithic rocks shift displacements, stresses and anomalous gravity field distributions around earthquake centre had a universal character. Those are not dependent on the thickness of elastic lithosphere, on the geological composition and linear dimensions of the earthquake centre. At the same time fracturing of geological rocks leads to the qualitative changes on the distribution patterns. Some irregular maximum and minimum zones can be seen. Their number grows as the rock fracturing increases. 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Stress-deformable state and anomalous gravity field in the earthquake centre with displacement along fault spread were modeled on the base of variation finite element method elaborated for elastic foliated shells. It was shown that in the case of monolithic rocks shift displacements, stresses and anomalous gravity field distributions around earthquake centre had a universal character. Those are not dependent on the thickness of elastic lithosphere, on the geological composition and linear dimensions of the earthquake centre. At the same time fracturing of geological rocks leads to the qualitative changes on the distribution patterns. Some irregular maximum and minimum zones can be seen. Their number grows as the rock fracturing increases. 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