{"id":3131,"date":"2015-03-23T15:32:08","date_gmt":"2015-03-23T13:32:08","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=3131"},"modified":"2015-03-24T09:18:30","modified_gmt":"2015-03-24T07:18:30","slug":"3131-2","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/3131-2\/","title":{"rendered":"2010; 1 : 22-32"},"content":{"rendered":"<p>Geoinformatika 2010; 1 :\u00a022-32<\/p>\n<h4>ABOUT POSSIBILITY OF HYDROCARBON ACCUMULATIONS MAPPING IN CRYSTALLINE ROCKS BY GEOELECTRIC METHODS<\/h4>\n<h5><em>Levashov S.P., Yakymchuk N.A., Korchagin I.N., Razin D.V., Juzlenko A.T.<\/em><\/h5>\n<p style=\"text-align: justify;\">The practical experience of experimental application in 2009 of untraditional geoelectric methods of forming short-pulsed electromagnetic field (FSPEF) and vertical electric-resonance sounding (VERS) (FSPEF\u2013VERS express-technology) on the local area of Novokonstsantinovskaya fracture zones within Ukrainian\u00a0 crystalline shield are given. The three anomalous geoelectric zones of 3.2 km<sup>2<\/sup>\u00a0area of gas (gas-condensate) type were revealed and mapped on investigation area by FSPEF method survey. The bedding depths of the anomalous polarized layers (APL) of gas and gas-condensate type were determined by VERS sounding. The anomalous zones are fixed along the general tectonic fractures. The revealed APL of gas and gas-condensate type in vertical cross-section are parallel to the tectonic fractures. The optimal places for the degassing borehole locations were delineated according to the measurement data by the FSPEF\u2013VERS methods. The local anomalous zone of \u201curanium mineralization area\u201d type was revealed and mapped by FSPEF method survey with the special antenna using. The experiment results testify of practical possibility of the FSPEF\u2013VERS technology using for the hydrocarbon accumulations exploration and prospecting in tectonically fractured zones of crystalline basement, as well as they are one more solid argument for the practicability of more broad using of FSPEF\u2013VERS methods in geological prospecting process for oil and gas.<\/p>\n<p style=\"text-align: justify;\"><strong>Keywords: <\/strong>geoelectric survey, electric-resonance sounding, deposit type anomaly, gas, gas-condensate, uranium mineralization, hydrocarbon accumulation, fracture zone, crystalline massif, basement.<\/p>\n<p><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2014\/09\/02_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><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2010; 1 :\u00a022-32 ABOUT POSSIBILITY OF HYDROCARBON ACCUMULATIONS MAPPING IN CRYSTALLINE ROCKS BY GEOELECTRIC METHODS Levashov S.P., Yakymchuk N.A., Korchagin I.N., Razin D.V., Juzlenko A.T. The practical experience of experimental application in 2009 of untraditional geoelectric methods of forming short-pulsed electromagnetic field (FSPEF) and vertical electric-resonance sounding (VERS) (FSPEF\u2013VERS express-technology) on the local area of Novokonstsantinovskaya fracture zones within Ukrainian\u00a0 crystalline shield are given. The three anomalous geoelectric zones of 3.2 km2\u00a0area of gas (gas-condensate) type were revealed and mapped on investigation area by FSPEF method survey. The bedding depths of the anomalous polarized layers (APL) of gas and gas-condensate type were determined by VERS sounding. The anomalous zones are fixed along the general tectonic fractures. The revealed APL of gas and gas-condensate type in vertical cross-section are parallel to the tectonic fractures. The optimal places for the degassing borehole locations were delineated according to the measurement data by the FSPEF\u2013VERS methods. The local anomalous zone of \u201curanium mineralization area\u201d type was revealed and mapped by FSPEF method survey with the special antenna using. The experiment results testify of practical possibility of the FSPEF\u2013VERS technology using for the hydrocarbon accumulations exploration and prospecting in tectonically fractured zones of crystalline basement, as well as they are one more solid argument for the practicability of more broad using of FSPEF\u2013VERS methods in geological prospecting process for oil and gas. Keywords: geoelectric survey, electric-resonance sounding, deposit type anomaly, gas, gas-condensate, uranium mineralization, hydrocarbon accumulation, fracture zone, crystalline massif, basement.<\/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-3131","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>2010; 1 : 22-32 - \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\/3131-2\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"2010; 1 : 22-32 - \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 2010; 1 :\u00a022-32 ABOUT POSSIBILITY OF HYDROCARBON ACCUMULATIONS MAPPING IN CRYSTALLINE ROCKS BY GEOELECTRIC METHODS Levashov S.P., Yakymchuk N.A., Korchagin I.N., Razin D.V., Juzlenko A.T. The practical experience of experimental application in 2009 of untraditional geoelectric methods of forming short-pulsed electromagnetic field (FSPEF) and vertical electric-resonance sounding (VERS) (FSPEF\u2013VERS express-technology) on the local area of Novokonstsantinovskaya fracture zones within Ukrainian\u00a0 crystalline shield are given. The three anomalous geoelectric zones of 3.2 km2\u00a0area of gas (gas-condensate) type were revealed and mapped on investigation area by FSPEF method survey. The bedding depths of the anomalous polarized layers (APL) of gas and gas-condensate type were determined by VERS sounding. The anomalous zones are fixed along the general tectonic fractures. The revealed APL of gas and gas-condensate type in vertical cross-section are parallel to the tectonic fractures. The optimal places for the degassing borehole locations were delineated according to the measurement data by the FSPEF\u2013VERS methods. The local anomalous zone of \u201curanium mineralization area\u201d type was revealed and mapped by FSPEF method survey with the special antenna using. The experiment results testify of practical possibility of the FSPEF\u2013VERS technology using for the hydrocarbon accumulations exploration and prospecting in tectonically fractured zones of crystalline basement, as well as they are one more solid argument for the practicability of more broad using of FSPEF\u2013VERS methods in geological prospecting process for oil and gas. Keywords: geoelectric survey, electric-resonance sounding, deposit type anomaly, gas, gas-condensate, uranium mineralization, hydrocarbon accumulation, fracture zone, crystalline massif, basement.\" \/>\n<meta property=\"og:url\" content=\"http:\/\/www.geology.com.ua\/en\/3131-2\/\" \/>\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=\"2015-03-24T07:18:30+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\\\/3131-2\\\/\",\"url\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/3131-2\\\/\",\"name\":\"2010; 1 : 22-32 - \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\\\/3131-2\\\/#primaryimage\"},\"image\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/3131-2\\\/#primaryimage\"},\"thumbnailUrl\":\"http:\\\/\\\/www.geology.com.ua\\\/wp-content\\\/uploads\\\/2013\\\/09\\\/pdf.jpg\",\"datePublished\":\"2015-03-23T13:32:08+00:00\",\"dateModified\":\"2015-03-24T07:18:30+00:00\",\"breadcrumb\":{\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/3131-2\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[[\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/3131-2\\\/\"]]}]},{\"@type\":\"ImageObject\",\"inLanguage\":\"en-US\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/3131-2\\\/#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\":\"BreadcrumbList\",\"@id\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/3131-2\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"http:\\\/\\\/www.geology.com.ua\\\/en\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"2010; 1 : 22-32\"}]},{\"@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":"2010; 1 : 22-32 - \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\/3131-2\/","og_locale":"en_US","og_type":"article","og_title":"2010; 1 : 22-32 - \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 2010; 1 :\u00a022-32 ABOUT POSSIBILITY OF HYDROCARBON ACCUMULATIONS MAPPING IN CRYSTALLINE ROCKS BY GEOELECTRIC METHODS Levashov S.P., Yakymchuk N.A., Korchagin I.N., Razin D.V., Juzlenko A.T. The practical experience of experimental application in 2009 of untraditional geoelectric methods of forming short-pulsed electromagnetic field (FSPEF) and vertical electric-resonance sounding (VERS) (FSPEF\u2013VERS express-technology) on the local area of Novokonstsantinovskaya fracture zones within Ukrainian\u00a0 crystalline shield are given. The three anomalous geoelectric zones of 3.2 km2\u00a0area of gas (gas-condensate) type were revealed and mapped on investigation area by FSPEF method survey. The bedding depths of the anomalous polarized layers (APL) of gas and gas-condensate type were determined by VERS sounding. The anomalous zones are fixed along the general tectonic fractures. The revealed APL of gas and gas-condensate type in vertical cross-section are parallel to the tectonic fractures. The optimal places for the degassing borehole locations were delineated according to the measurement data by the FSPEF\u2013VERS methods. The local anomalous zone of \u201curanium mineralization area\u201d type was revealed and mapped by FSPEF method survey with the special antenna using. The experiment results testify of practical possibility of the FSPEF\u2013VERS technology using for the hydrocarbon accumulations exploration and prospecting in tectonically fractured zones of crystalline basement, as well as they are one more solid argument for the practicability of more broad using of FSPEF\u2013VERS methods in geological prospecting process for oil and gas. Keywords: geoelectric survey, electric-resonance sounding, deposit type anomaly, gas, gas-condensate, uranium mineralization, hydrocarbon accumulation, fracture zone, crystalline massif, basement.","og_url":"http:\/\/www.geology.com.ua\/en\/3131-2\/","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":"2015-03-24T07:18:30+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\/3131-2\/","url":"http:\/\/www.geology.com.ua\/en\/3131-2\/","name":"2010; 1 : 22-32 - \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\/3131-2\/#primaryimage"},"image":{"@id":"http:\/\/www.geology.com.ua\/en\/3131-2\/#primaryimage"},"thumbnailUrl":"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2013\/09\/pdf.jpg","datePublished":"2015-03-23T13:32:08+00:00","dateModified":"2015-03-24T07:18:30+00:00","breadcrumb":{"@id":"http:\/\/www.geology.com.ua\/en\/3131-2\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":[["http:\/\/www.geology.com.ua\/en\/3131-2\/"]]}]},{"@type":"ImageObject","inLanguage":"en-US","@id":"http:\/\/www.geology.com.ua\/en\/3131-2\/#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":"BreadcrumbList","@id":"http:\/\/www.geology.com.ua\/en\/3131-2\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"http:\/\/www.geology.com.ua\/en\/"},{"@type":"ListItem","position":2,"name":"2010; 1 : 22-32"}]},{"@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\/3131","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=3131"}],"version-history":[{"count":2,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/3131\/revisions"}],"predecessor-version":[{"id":3134,"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/pages\/3131\/revisions\/3134"}],"wp:attachment":[{"href":"http:\/\/www.geology.com.ua\/en\/wp-json\/wp\/v2\/media?parent=3131"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}