{"id":6127,"date":"2016-09-21T10:18:55","date_gmt":"2016-09-21T08:18:55","guid":{"rendered":"http:\/\/www.geology.com.ua\/?page_id=6127"},"modified":"2021-06-21T18:29:53","modified_gmt":"2021-06-21T16:29:53","slug":"geoinformatika-2016-359-14-19","status":"publish","type":"page","link":"http:\/\/www.geology.com.ua\/en\/geoinformatika-2016-359-14-19\/","title":{"rendered":"Geoinformatika 2016; 3(59) : 14-19"},"content":{"rendered":"<p><em>Geoinformatika 2016; 3(59) : 14-19 \u00a0<\/em><em>(in Ukrainian)<\/em><\/p>\n<h4>Paleo-Channels Prediction in Carboniferous Sediments of the South-East Part of the Dnieper-Donets Basin (Based on the Results of Siesmic-Facies Analysis)<\/h4>\n<h5><em>N.I. Nesina, G.G. Markova<\/em><\/h5>\n<p style=\"text-align: justify\"><em>LLC \u201cVikoil LTD\u201d, 7 Kudryavsky uzviz Str., of. 920, Kyiv 04053, Ukraine, e-mail: natalia_nesina@bigmir.net, galina.markova@ubseismic.com<\/em><\/p>\n<p style=\"text-align: justify\">The<strong> purpose <\/strong>of the paper is to show the efficacy of seismic-facies analysis for more specific application of 3D seismic to predict lithological hydrocarbon traps. The analysis was carried out in the South-East part of the Dnieper-Donets Basin for the sediments of Carboneferous on the sides of an anticline fold formed during a salt dome structure growing.<br \/>\n<strong>Design\/methodology\/approach. <\/strong>Predictions were carried out using Neural Network Technology (NNT) seismic traces classification to obtain seismic facies distribution.<br \/>\n<strong>Findings.<\/strong> The prediction areas of paleo-channels location were identified in the intervals of the Middle and Upper Carboniferous sediments based on the results of seismic-facies analysis. The results of the seismic-facies maps analysis, vertical sections and horizon slices of the seismic cube with amplitude anomalies corresponding to paleo-channels, allowed us to suppose that these paleo-channels were formed under different conditions of sedimentation. These conditions were connected with global sea level variations and with local tectonic movements caused by salt-dome structure forming.<br \/>\n<strong>Practical value\/implications. <\/strong>Paleo-channels, as the lithological bodies, are quite promising for potential non-anticline hydrocarbon traps forming. The latter has been constantly confirmed by Ukrainian and foreign geologists.<\/p>\n<p style=\"text-align: justify\"><strong>Keywords:<\/strong> seismic-facies analysis, paleo-channel, horizon slice, Dnieper-Donets Basin, Pennsylvanian.<\/p>\n<p style=\"text-align: justify\"><span style=\"color: #0000ff\"><em><strong><a href=\"http:\/\/www.geology.com.ua\/wp-content\/uploads\/2021\/06\/Geo-3-2016-14-19.pdf\"><span style=\"color: #0000ff\">The full text of papers <\/span><\/a> <\/strong><\/em><\/span><\/p>\n<p style=\"text-align: justify\"><strong><\/p>\n<ul class='gdl-toggle-box'>\r\n<li class=''><h2 class='toggle-box-title'>References:<\/h2><div class='toggle-box-content'><p><\/strong><\/p>\n<ol>\n<li style=\"text-align: justify\">Atlas rodovyshch nafty i hazu Ukrayiny. M.M. Ivanyuta, V.O.Fedyshyn, B.I. Deneha. L\u2019viv, UNHA, 1998, 1421 p. (in Ukrainian).<\/li>\n<li style=\"text-align: justify\">Geologicheskaja istorija territorii Ukrainy. Paleozoj. O.I. Berchenko, N.I. Bojarina, G.I. Vakarchuk. Kyiv, Naukova dumka, 1993, 199 p. (in Russian).<\/li>\n<li style=\"text-align: justify\">Geologija i neftegazonosnost\u2019 Dneprovsko-Doneckoj vpadiny. Stratigrafija. D.E. Ajzenverg, O.I. Berchenko, N.E. Brazhnikova. Kyiv, Naukova dumka, 1988, 148 p. (in Russian).<\/li>\n<li style=\"text-align: justify\">Lukin A.E., Korzhnev P.M., Naumenko A.D., Okrepkij S.V. Problema facial\u2019noj diagnostiki peschanyh tel i puti ee reshe\u00adnija. <em>Geologicheskij zhurnal<\/em>, 2012, no. 2, pp. 7-21 (in Russian).<\/li>\n<li style=\"text-align: justify\">Nesina N., Zdorovenko M., Shkrob T., Dyachenko K. Vizeys\u2019kyy karbonatnyy masyv na Lyvens\u2019kiy strukturi (tsentral\u2019na chastyna pivdennoyi prybortovoyi zony Dniprovs\u2019ko-Donets\u2019koyi zapadyny). <em>Ukrainian Geologist<\/em>, 2012, no. 1, pp. 83-86. (in Ukrainian).<\/li>\n<li style=\"text-align: justify\">Nesina N.I. Zastosuvanya seysmofatsial\u2019noho analizu dlya vyvchennya verkhn\u2019oserpukhovs\u2019kykh vidkladiv Sukhodol\u2019s\u2019koyi ploshchi (pivnichni okrayiny Donbasu). <em>Zbirnyk naukovykh prats\u2019 UkrNDI HRI<\/em>, 2012, no. 4, pp. 184-188 (in Ukrainian).<\/li>\n<li style=\"text-align: justify\">Nesina N.I. Primenenie rezul\u2019tatov sejsmofacial\u2019nogo analiza v komplekse s dannymi burenija i GIS dlja prognoza neantiklinal\u2019nyh lovushek uglevodorodov v central\u2019noj chasti Severnogo borta Dneprovsko-Doneckoj vpadiny. <em>Azerbaijan Geologist<\/em>, 2013, no. 17, pp. 101-108 (in Russian).<\/li>\n<li style=\"text-align: justify\">Nezhdanov A.A. Geologicheskaja interpretacija sejsmorazvedochnyh dannyh. Tjumen\u2019, Tjumenskij gosudarstvennyj neftegazovyj universitet, 2000, 133 p.<br \/>\n(in Russian).<\/li>\n<li style=\"text-align: justify\">Khabanets I.A., Tiapkina O.M. Seismic image prediction and classification of upper serpukhovian carbonate buildups. <em>Geoinformatika<\/em>, 2015, no. 2, pp. 62-70<br \/>\n(in Ukrainian).<\/li>\n<li style=\"text-align: justify\">Shakin V.A. Zony neftegazonakpolenija Dneprovsko-Doneckoj vpadiny. Moskow, Nedra, 1977, 120 p.<\/li>\n<li style=\"text-align: justify\">Krawczynski L. Sequence stratigraphic interpretation integrated with 3D seismic attribute analysis in an intracratonic setting: Toolachee formation, Cooper Basin, Australia: Master\u2019s Thesis. Queensland, Queensland University of Technology, School of Natural Resource Sciences, 2004, 186 p.<\/li>\n<li style=\"text-align: justify\">Shikhaliyev A., Sadykhov S.D. Lithology, facies and structural features study based on seismic and well data: methodology and applicaton. <em>Geophysics News in Azerbaijan<\/em>, 2007, no. 1, p. 5-11.<\/li>\n<li style=\"text-align: justify\">Skirius C., Nissen S., Haskell N. 3D seismic attributes applied to carbonates. <em>The Leading Edge<\/em>, 1999, no. l, pp. 384-393.<\/li>\n<\/ol>\n<p><strong>\u00a0<\/p>\n<\/div><\/li> <\/ul>\n<p> <\/strong><\/p>","protected":false},"excerpt":{"rendered":"<p>Geoinformatika 2016; 3(59) : 14-19 \u00a0(in Ukrainian) Paleo-Channels Prediction in Carboniferous Sediments of the South-East Part of the Dnieper-Donets Basin (Based on the Results of Siesmic-Facies Analysis) N.I. Nesina, G.G. Markova LLC \u201cVikoil LTD\u201d, 7 Kudryavsky uzviz Str., of. 920, Kyiv 04053, Ukraine, e-mail: natalia_nesina@bigmir.net, galina.markova@ubseismic.com The purpose of the paper is to show the efficacy of seismic-facies analysis for more specific application of 3D seismic to predict lithological hydrocarbon traps. The analysis was carried out in the South-East part of the Dnieper-Donets Basin for the sediments of Carboneferous on the sides of an anticline fold formed during a salt dome structure growing. Design\/methodology\/approach. Predictions were carried out using Neural Network Technology (NNT) seismic traces classification to obtain seismic facies distribution. Findings. The prediction areas of paleo-channels location were identified in the intervals of the Middle and Upper Carboniferous sediments based on the results of seismic-facies analysis. The results of the seismic-facies maps analysis, vertical sections and horizon slices of the seismic cube with amplitude anomalies corresponding to paleo-channels, allowed us to suppose that these paleo-channels were formed under different conditions of sedimentation. These conditions were connected with global sea level variations and with local tectonic movements caused by salt-dome structure forming. Practical value\/implications. Paleo-channels, as the lithological bodies, are quite promising for potential non-anticline hydrocarbon traps forming. The latter has been constantly confirmed by Ukrainian and foreign geologists. Keywords: seismic-facies analysis, paleo-channel, horizon slice, Dnieper-Donets Basin, Pennsylvanian. The full text of papers<\/p>\n","protected":false},"author":2,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-6127","page","type-page","status-publish","hentry"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v27.5 - https:\/\/yoast.com\/product\/yoast-seo-wordpress\/ -->\n<title>Geoinformatika 2016; 3(59) : 14-19 - \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\/geoinformatika-2016-359-14-19\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Geoinformatika 2016; 3(59) : 14-19 - \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 2016; 3(59) : 14-19 \u00a0(in Ukrainian) Paleo-Channels Prediction in Carboniferous Sediments of the South-East Part of the Dnieper-Donets Basin (Based on the Results of Siesmic-Facies Analysis) N.I. Nesina, G.G. Markova LLC \u201cVikoil LTD\u201d, 7 Kudryavsky uzviz Str., of. 920, Kyiv 04053, Ukraine, e-mail: natalia_nesina@bigmir.net, galina.markova@ubseismic.com The purpose of the paper is to show the efficacy of seismic-facies analysis for more specific application of 3D seismic to predict lithological hydrocarbon traps. The analysis was carried out in the South-East part of the Dnieper-Donets Basin for the sediments of Carboneferous on the sides of an anticline fold formed during a salt dome structure growing. Design\/methodology\/approach. Predictions were carried out using Neural Network Technology (NNT) seismic traces classification to obtain seismic facies distribution. Findings. The prediction areas of paleo-channels location were identified in the intervals of the Middle and Upper Carboniferous sediments based on the results of seismic-facies analysis. The results of the seismic-facies maps analysis, vertical sections and horizon slices of the seismic cube with amplitude anomalies corresponding to paleo-channels, allowed us to suppose that these paleo-channels were formed under different conditions of sedimentation. These conditions were connected with global sea level variations and with local tectonic movements caused by salt-dome structure forming. Practical value\/implications. Paleo-channels, as the lithological bodies, are quite promising for potential non-anticline hydrocarbon traps forming. The latter has been constantly confirmed by Ukrainian and foreign geologists. Keywords: seismic-facies analysis, paleo-channel, horizon slice, Dnieper-Donets Basin, Pennsylvanian. 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Nesina, G.G. Markova LLC \u201cVikoil LTD\u201d, 7 Kudryavsky uzviz Str., of. 920, Kyiv 04053, Ukraine, e-mail: natalia_nesina@bigmir.net, galina.markova@ubseismic.com The purpose of the paper is to show the efficacy of seismic-facies analysis for more specific application of 3D seismic to predict lithological hydrocarbon traps. The analysis was carried out in the South-East part of the Dnieper-Donets Basin for the sediments of Carboneferous on the sides of an anticline fold formed during a salt dome structure growing. Design\/methodology\/approach. Predictions were carried out using Neural Network Technology (NNT) seismic traces classification to obtain seismic facies distribution. Findings. The prediction areas of paleo-channels location were identified in the intervals of the Middle and Upper Carboniferous sediments based on the results of seismic-facies analysis. The results of the seismic-facies maps analysis, vertical sections and horizon slices of the seismic cube with amplitude anomalies corresponding to paleo-channels, allowed us to suppose that these paleo-channels were formed under different conditions of sedimentation. These conditions were connected with global sea level variations and with local tectonic movements caused by salt-dome structure forming. Practical value\/implications. Paleo-channels, as the lithological bodies, are quite promising for potential non-anticline hydrocarbon traps forming. The latter has been constantly confirmed by Ukrainian and foreign geologists. Keywords: seismic-facies analysis, paleo-channel, horizon slice, Dnieper-Donets Basin, Pennsylvanian. 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