{"id":1936,"date":"2020-10-27T21:21:44","date_gmt":"2020-10-27T18:21:44","guid":{"rendered":"https:\/\/adcr.ru\/?p=1936"},"modified":"2020-10-27T21:25:10","modified_gmt":"2020-10-27T18:25:10","slug":"2017-2-4","status":"publish","type":"post","link":"https:\/\/adcr.ru\/en\/2017-2-4\/","title":{"rendered":"\"REPORTER of the Association of Drilling Contractors\" \u21162, 2017"},"content":{"rendered":"
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NEW VIEWS ABOUT THE STRUCTURE OF THE LATE DEVONIAN \u2014 EARLY CARBONIFEROUS REEF FORMATIONS OF THE NIKOLAYEVO-GORODISHCHENSKY STAGE<\/strong>

Danshina N.V. \u2013 Candidate of Geological and Mineralogical Sciences, Leading Researcher of the Oil and Gas Prediction Laboratory, Senior Research in the field of Paleontology and Stratigraphy, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, ndanshina@lukoilvmn.ru ndanshina@lukoilvmn.ru<\/a>
Medvedeva E.P. \u2013 Head of the oil and gas Prediction Laboratory, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, emedvedeva@lukoilvmn.ru emedvedeva@lukoilvmn.ru<\/a>
Makhonin M.V. \u2013 Head of the Department for Monitoring and Design of Geological Exploration Work, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, mmakhonin@lukoilvmn.ru mmakhonin@lukoilvmn.ru<\/a>
Androsenko T.O. - Engineer of the Oil and Gas Potential Forecasting Laboratory, VolgogradNIPImorneft branch of OOO LUKOIL-Engineering,tandrosenko@lukoilvmn.ru tandrosenko@lukoilvmn.ru<\/a>

<\/em><\/strong>\u0423\u0414\u041a 5 552.5+551.8+551.3.051+551.734+553.98(470.45)

Key words: <\/strong>wells; Carbonate deposits; microbial Limestones; Detrital-algae; Complex of organic remains; Micrite Walsoort domes.

The article is devoted to a description of the Core Material from the wells of the Late Paleozoic reefogenic formations of the Volgograd Trans-Volga region. Sections of wells 1, 2 Novo-Dmitrievskiy, drilled in 2014-2016, have revealed productive Famennian-Turney organogenic structures (Walsort facies). The main stages of the unique reef formations-the Walsoort facies-are singled out. For the first time in the history of the region in the reef facies of roofing layers of the Famennian stage of the Upper Devonian traced deposits of an additional Zygansk horizon, which was not traced in layered sections. Complexes of sediments on real wells are given.<\/p>\n

NEW VIEWS ABOUT THE STRUCTURE OF THE LATE DEVONIAN — EARLY CARBONIFEROUS REEF FORMATIONS OF THE NIKOLAYEVO-GORODISHCHENSKY STAGE

Danshina N.V. \u2013 Candidate of Geological and Mineralogical Sciences, Leading Researcher of the Oil and Gas Prediction Laboratory, Senior Research in the field of Paleontology and Stratigraphy, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, ndanshina@lukoilvmn.ru<\/a>
\u0415\u043b\u0435\u043d\u0430 \u041f\u0435\u0442\u0440\u043e\u0432\u043d\u0430 \u041c\u0435\u0434\u0432\u0435\u0434\u0435\u0432\u0430 \u2013 \u0437\u0430\u0432. \u043b\u0430\u0431\u043e\u0440\u0430\u0442\u043e\u0440\u0438\u0435\u0439 \u043f\u0440\u043e\u0433\u043d\u043e\u0437\u0438\u0440\u043e\u0432\u0430\u043d\u0438\u044f \u043d\u0435\u0444\u0442\u0435\u0433\u0430\u0437\u043e\u043d\u043e\u0441\u043d\u043e\u0441\u0442\u0438, \u0444\u0438\u043b\u0438\u0430\u043b \u041e\u041e\u041e \u00ab\u041b\u0423\u041a\u041e\u0419\u041b-\u0438\u043d\u0436\u0438\u043d\u0438\u0440\u0438\u043d\u0433\u00bb \u00ab\u0412\u043e\u043b\u0433\u043e\u0433\u0440\u0430\u0434\u041d\u0418\u041f\u0418\u043c\u043e\u0440\u043d\u0435\u0444\u0442\u044c\u00bbMedvedeva E.P. \u2013 Head of the oil and gas Prediction Laboratory, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, emedvedeva@lukoilvmn.ru<\/a>
Makhonin M.V. \u2013 Head of the Department for Monitoring and Design of Geological Exploration Work, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, mmakhonin@lukoilvmn.ru<\/a>
Makhonin M.V. \u2013 Head of the Department for Monitoring and Design of Geological Exploration Work, Branch of LLC LUKOIL-Engineering VolgogradNIPImorneft, tandrosenko@lukoilvmn.ru<\/a>
<\/em><\/strong>
Key words: <\/strong>wells; Carbonate deposits; microbial Limestones; Detrital-algae; Complex of organic remains; Micrite Walsoort domes.

The article is devoted to a description of the Core Material from the wells of the Late Paleozoic reefogenic formations of the Volgograd Trans-Volga region. Sections of wells 1, 2 Novo-Dmitrievskiy, drilled in 2014-2016, have revealed productive Famennian-Turney organogenic structures (Walsort facies). The main stages of the unique reef formations-the Walsoort facies-are singled out. For the first time in the history of the region in the reef facies of roofing layers of the Famennian stage of the Upper Devonian traced deposits of an additional Zygansk horizon, which was not traced in layered sections. Complexes of sediments on real wells are given.<\/p>\n

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