{"id":3265,"date":"2015-03-25T12:53:37","date_gmt":"2015-03-25T10:53:37","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3265"},"modified":"2015-03-25T12:53:37","modified_gmt":"2015-03-25T10:53:37","slug":"2009-3-59-67","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2009-3-59-67\/","title":{"rendered":"2009; 3 : 59-67"},"content":{"rendered":"<p>Geoinformatika 2009; 3 :\u00a059-67<\/p>\n<h4>\u201cGRAVITATIONAL TOMOGRAPHY\u201d \u2013 PRACTICE OVERTAKING THEORY?<\/h4>\n<h5><em>Dolgal A.S., Sharhimullin A.F.<\/em><\/h5>\n<p style=\"text-align: justify;\">This paper considers a number of questions, connected with \u201cgravitational tomography\u201d \u2013 a line in interpretation, aimed at getting space distribution of density in a studied volume of geological environment without using classical inverse problem methods of\u00a0 gravimetry. Examples of algorithms and interpretating schemata are given. An attempt of considering \u201cgravitational tomography\u201d from the positions of geoimage data processing theory is made. Directions of further research are offered.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/Dolgal.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 :\u00a059-67 \u201cGRAVITATIONAL TOMOGRAPHY\u201d \u2013 PRACTICE OVERTAKING THEORY? Dolgal A.S., Sharhimullin A.F. This paper considers a number of questions, connected with \u201cgravitational tomography\u201d \u2013 a line in interpretation, aimed at getting space distribution of density in a studied volume of geological environment without using classical inverse problem methods of\u00a0 gravimetry. Examples of algorithms and interpretating schemata are given. An attempt of considering \u201cgravitational tomography\u201d from the positions of geoimage data processing theory is made. Directions of further research are offered.<\/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-3265","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 : 59-67 - \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\/2009-3-59-67\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2009; 3 : 59-67 - \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 :\u00a059-67 \u201cGRAVITATIONAL TOMOGRAPHY\u201d \u2013 PRACTICE OVERTAKING THEORY? Dolgal A.S., Sharhimullin A.F. This paper considers a number of questions, connected with \u201cgravitational tomography\u201d \u2013 a line in interpretation, aimed at getting space distribution of density in a studied volume of geological environment without using classical inverse problem methods of\u00a0 gravimetry. Examples of algorithms and interpretating schemata are given. An attempt of considering \u201cgravitational tomography\u201d from the positions of geoimage data processing theory is made. 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