{"id":3311,"date":"2015-03-27T11:07:28","date_gmt":"2015-03-27T09:07:28","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3311"},"modified":"2015-03-27T11:07:28","modified_gmt":"2015-03-27T09:07:28","slug":"2009-2-71-79","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2009-2-71-79\/","title":{"rendered":"2009; 2 : 71-79"},"content":{"rendered":"<p>Geoinformatika 2009; 2 :\u00a071-79<\/p>\n<h4>LANDSCAPE GEOINDICATORS OF THE FRACTURES&#8217; DESCRIPTIONS AS THE FOUNDATION OF THEIR INVESTIGATION VIA REMOTE SENSING METHODS. 2. GEODYNAMIC FEATURES OF THE DISJUNCTIVE STRUCTURES<\/h4>\n<h5><em>Azimov O.T.<\/em><\/h5>\n<p style=\"text-align: justify;\">For the conditions of the platform areas there are characterised the basic landscape features of the discriminating geodynamic fields at the recent tectogenesis stage. The fields are related to the Earth\u2019s crust disjunctive structures. Peculiarities of the fields&#8217; reflection in the remote sensing data are described too.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/Azimov.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; 2 :\u00a071-79 LANDSCAPE GEOINDICATORS OF THE FRACTURES&#8217; DESCRIPTIONS AS THE FOUNDATION OF THEIR INVESTIGATION VIA REMOTE SENSING METHODS. 2. GEODYNAMIC FEATURES OF THE DISJUNCTIVE STRUCTURES Azimov O.T. For the conditions of the platform areas there are characterised the basic landscape features of the discriminating geodynamic fields at the recent tectogenesis stage. The fields are related to the Earth\u2019s crust disjunctive structures. Peculiarities of the fields&#8217; reflection in the remote sensing data are described too.<\/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-3311","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; 2 : 71-79 - \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\/2009-2-71-79\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2009; 2 : 71-79 - \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; 2 :\u00a071-79 LANDSCAPE GEOINDICATORS OF THE FRACTURES&#8217; DESCRIPTIONS AS THE FOUNDATION OF THEIR INVESTIGATION VIA REMOTE SENSING METHODS. 2. GEODYNAMIC FEATURES OF THE DISJUNCTIVE STRUCTURES Azimov O.T. For the conditions of the platform areas there are characterised the basic landscape features of the discriminating geodynamic fields at the recent tectogenesis stage. The fields are related to the Earth\u2019s crust disjunctive structures. 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GEODYNAMIC FEATURES OF THE DISJUNCTIVE STRUCTURES Azimov O.T. For the conditions of the platform areas there are characterised the basic landscape features of the discriminating geodynamic fields at the recent tectogenesis stage. The fields are related to the Earth\u2019s crust disjunctive structures. 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