{"id":2278,"date":"2015-02-06T11:38:54","date_gmt":"2015-02-06T09:38:54","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=2278"},"modified":"2015-09-01T09:24:43","modified_gmt":"2015-09-01T07:24:43","slug":"2278-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/2278-2\/","title":{"rendered":""},"content":{"rendered":"<p>Geoinformatika 2013; 4(48) :\u00a05-16<\/p>\n<h4>THE SOUTH FALKLAND BASIN: NEW DATA ON DEEP GEOPHYSICAL INHOMOGENEITIES\u00a0AND OIL AND GAS POTENTIAL (BASED ON REMOTE SENSING AND GEOELECTRIC RESULTS)<\/h4>\n<h5><em>S.P. Levashov, N.A. Yakymchuk, I.N. Korchagin, Yu.M. Pischany, V.G. Bakhmutov, V.D. Solovyov, D.N. Bozhezha<\/em><\/h5>\n<p style=\"text-align: justify;\">\u00a0Geoelectric measurements made during the 17th\u00a0Ukrainian Antarctic Expedition (XVII UAE, 2012) allowed to obtain new results on the deep structure of the tectonic zone between the Falkland Islands and the South Shetland Islands. The results make it possible to estimate the probable nature of geodynamic processes in this region. Deep geoelectric boundaries position and the nature of their contacts near the South Shetland Islands and the Falkland Islands show a fundamentally different distribution of the crustal and mantle homogeneities in the Strait structures forming continental and oceanic rock complexes. In the South Falkland Basin shelf, some anomalous zones of \u201chydrocarbon deposit\u201d type were detected due to special technology of satellite data processing and interpretation. The \u201cdeposit\u201d type anomalies were mapped by FSPEF survey and anomalous polarized layers of \u201cthe hydrocarbon deposit\u201d type were chosen by VERS sounding within these anomalies. These result contribute in the oil and gas potential data for the South Falkland Basin shelf zone.<\/p>\n<p style=\"text-align: justify;\"><strong>Keywords:<\/strong> South Falkland Basin region, remote data processing, geoelectric survey, deep structure, hydrocarbons.<\/p>\n<p style=\"text-align: justify;\"><em><strong><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2015\/08\/01_Levashov.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>\n<p><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2013; 4(48) :\u00a05-16 THE SOUTH FALKLAND BASIN: NEW DATA ON DEEP GEOPHYSICAL INHOMOGENEITIES\u00a0AND OIL AND GAS POTENTIAL (BASED ON REMOTE SENSING AND GEOELECTRIC RESULTS) S.P. Levashov, N.A. Yakymchuk, I.N. Korchagin, Yu.M. Pischany, V.G. Bakhmutov, V.D. Solovyov, D.N. Bozhezha \u00a0Geoelectric measurements made during the 17th\u00a0Ukrainian Antarctic Expedition (XVII UAE, 2012) allowed to obtain new results on the deep structure of the tectonic zone between the Falkland Islands and the South Shetland Islands. The results make it possible to estimate the probable nature of geodynamic processes in this region. Deep geoelectric boundaries position and the nature of their contacts near the South Shetland Islands and the Falkland Islands show a fundamentally different distribution of the crustal and mantle homogeneities in the Strait structures forming continental and oceanic rock complexes. In the South Falkland Basin shelf, some anomalous zones of \u201chydrocarbon deposit\u201d type were detected due to special technology of satellite data processing and interpretation. The \u201cdeposit\u201d type anomalies were mapped by FSPEF survey and anomalous polarized layers of \u201cthe hydrocarbon deposit\u201d type were chosen by VERS sounding within these anomalies. These result contribute in the oil and gas potential data for the South Falkland Basin shelf zone. Keywords: South Falkland Basin region, remote data processing, geoelectric survey, deep structure, hydrocarbons.<\/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-2278","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.9 - 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\/2278-2\/\" \/>\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) :\u00a05-16 THE SOUTH FALKLAND BASIN: NEW DATA ON DEEP GEOPHYSICAL INHOMOGENEITIES\u00a0AND OIL AND GAS POTENTIAL (BASED ON REMOTE SENSING AND GEOELECTRIC RESULTS) S.P. Levashov, N.A. Yakymchuk, I.N. Korchagin, Yu.M. Pischany, V.G. Bakhmutov, V.D. Solovyov, D.N. Bozhezha \u00a0Geoelectric measurements made during the 17th\u00a0Ukrainian Antarctic Expedition (XVII UAE, 2012) allowed to obtain new results on the deep structure of the tectonic zone between the Falkland Islands and the South Shetland Islands. The results make it possible to estimate the probable nature of geodynamic processes in this region. Deep geoelectric boundaries position and the nature of their contacts near the South Shetland Islands and the Falkland Islands show a fundamentally different distribution of the crustal and mantle homogeneities in the Strait structures forming continental and oceanic rock complexes. In the South Falkland Basin shelf, some anomalous zones of \u201chydrocarbon deposit\u201d type were detected due to special technology of satellite data processing and interpretation. The \u201cdeposit\u201d type anomalies were mapped by FSPEF survey and anomalous polarized layers of \u201cthe hydrocarbon deposit\u201d type were chosen by VERS sounding within these anomalies. These result contribute in the oil and gas potential data for the South Falkland Basin shelf zone. Keywords: South Falkland Basin region, remote data processing, geoelectric survey, deep structure, hydrocarbons.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/2278-2\/\" \/>\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=\"2015-09-01T07:24:43+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\\\/2278-2\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2278-2\\\/\",\"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\\\/2278-2\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2278-2\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-02-06T09:38:54+00:00\",\"dateModified\":\"2015-09-01T07:24:43+00:00\",\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2278-2\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/2278-2\\\/#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\/2278-2\/","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) :\u00a05-16 THE SOUTH FALKLAND BASIN: NEW DATA ON DEEP GEOPHYSICAL INHOMOGENEITIES\u00a0AND OIL AND GAS POTENTIAL (BASED ON REMOTE SENSING AND GEOELECTRIC RESULTS) S.P. Levashov, N.A. Yakymchuk, I.N. Korchagin, Yu.M. Pischany, V.G. Bakhmutov, V.D. Solovyov, D.N. Bozhezha \u00a0Geoelectric measurements made during the 17th\u00a0Ukrainian Antarctic Expedition (XVII UAE, 2012) allowed to obtain new results on the deep structure of the tectonic zone between the Falkland Islands and the South Shetland Islands. The results make it possible to estimate the probable nature of geodynamic processes in this region. Deep geoelectric boundaries position and the nature of their contacts near the South Shetland Islands and the Falkland Islands show a fundamentally different distribution of the crustal and mantle homogeneities in the Strait structures forming continental and oceanic rock complexes. In the South Falkland Basin shelf, some anomalous zones of \u201chydrocarbon deposit\u201d type were detected due to special technology of satellite data processing and interpretation. The \u201cdeposit\u201d type anomalies were mapped by FSPEF survey and anomalous polarized layers of \u201cthe hydrocarbon deposit\u201d type were chosen by VERS sounding within these anomalies. These result contribute in the oil and gas potential data for the South Falkland Basin shelf zone. Keywords: South Falkland Basin region, remote data processing, geoelectric survey, deep structure, hydrocarbons.","og_url":"http:\/\/www.geology.com.ua\/en\/2278-2\/","og_site_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","article_modified_time":"2015-09-01T07:24:43+00:00","og_image":[{"url":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","type":"","width":"","height":""}],"twitter_misc":{"Est. reading time":"1 minute"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"http:\/\/www.geology.com.ua\/en\/2278-2\/","url":"http:\/\/www.geology.com.ua\/en\/2278-2\/","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\/2278-2\/#primaryimage"},"image":{"@id":"http:\/\/www.geology.com.ua\/en\/2278-2\/#primaryimage"},"thumbnailUrl":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","datePublished":"2015-02-06T09:38:54+00:00","dateModified":"2015-09-01T07:24:43+00:00","inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":[["http:\/\/www.geology.com.ua\/en\/2278-2\/"]]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"http:\/\/www.geology.com.ua\/en\/2278-2\/#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"}]}},"_links":{"self":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2278","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/comments?post=2278"}],"version-history":[{"count":4,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2278\/revisions"}],"predecessor-version":[{"id":4322,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/2278\/revisions\/4322"}],"wp:attachment":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/media?parent=2278"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}