{"id":3358,"date":"2015-03-30T11:29:23","date_gmt":"2015-03-30T09:29:23","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3358"},"modified":"2015-03-30T11:29:23","modified_gmt":"2015-03-30T09:29:23","slug":"2009-1-69-81","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2009-1-69-81\/","title":{"rendered":"2009; 1 : 69-81"},"content":{"rendered":"<p>Geoinformatika 2009; 1 :\u00a069-81<\/p>\n<h4>LANDSCAPE GEOINDICATORS OF FRACTURES&#8217; DESCRIPTIONS AS A FOUNDATION OF THEIR RESEARCH BY REMOTE SENSING METHODS. 1. MORPHOKINEMATIC FEATURES OF DISJUNCTIVE STRUCTURES<\/h4>\n<h5><em>Azimov O.T.<\/em><\/h5>\n<p style=\"text-align: justify;\">The article presents basic features of kinematic descriptions of the Earth&#8217;s crust disjunctive structures in the main constituent of the recent landscape for the day surface. There are also described peculiarities of reflecting the features in remote sensing data. The features are for conditions of platform areas.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/10\/\u043b\u0430\u043d\u0434\u0448\u0430\u0444\u0442\u043d\u0456-\u0433\u0435\u043e\u0456\u043d\u0434\u0438\u043a\u0430\u0442\u043e\u0440\u04382.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; 1 :\u00a069-81 LANDSCAPE GEOINDICATORS OF FRACTURES&#8217; DESCRIPTIONS AS A FOUNDATION OF THEIR RESEARCH BY REMOTE SENSING METHODS. 1. MORPHOKINEMATIC FEATURES OF DISJUNCTIVE STRUCTURES Azimov O.T. The article presents basic features of kinematic descriptions of the Earth&#8217;s crust disjunctive structures in the main constituent of the recent landscape for the day surface. There are also described peculiarities of reflecting the features in remote sensing data. The features are for conditions of platform areas.<\/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-3358","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; 1 : 69-81 - \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\/2009-1-69-81\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2009; 1 : 69-81 - \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; 1 :\u00a069-81 LANDSCAPE GEOINDICATORS OF FRACTURES&#8217; DESCRIPTIONS AS A FOUNDATION OF THEIR RESEARCH BY REMOTE SENSING METHODS. 1. MORPHOKINEMATIC FEATURES OF DISJUNCTIVE STRUCTURES Azimov O.T. The article presents basic features of kinematic descriptions of the Earth&#8217;s crust disjunctive structures in the main constituent of the recent landscape for the day surface. There are also described peculiarities of reflecting the features in remote sensing data. 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