GEOLOGICAL FEATURES OF FLUID ZONATION IN MULTILAYER FIELD OF DNIEPER-DONETSK DEPRESSION

Authors

  • В. М. Абєлєнцев Ukrainian Research Institute for Natural Gases, Ukraine
  • А. Й. Лур’є V.N. Karazin Kharkiv National University, Ukraine
  • Л. O. Міщенко Ukrainian Research Institute for Natural Gases, Ukraine

DOI:

https://doi.org/10.26565/2410-7360-2015-43-01

Keywords:

multilayer fields, fluid zoning, hydrocarbon deposits, oil-and-gas-bearing prospects

Abstract

Geological conditions of hydrocarbons occurrence in multilayer fields are reviewed to identify prospective underexplored areas on the example of North near-edge zone of Dnieper-Donetsk depression. The main factors of the geological structure multilayer fields as structural-tectonic, stratigraphic, lithofacies, morphological, filtration-capacitive, hydrogeological, thermobaric have been defined. Geological localization features of hydrocarbon deposits of multilayer fields in North near-edge zone of Dnieper-Donetsk depression were analyzed. According to the results of using the parameters of oil-and-gaz-saturation pore the volumes of hydrocarbon deposits were identified as well as features of hydrocarbon fields’ vertical zonation. This option more fully describes the internal, discrete structure of each of the fields. As a result of the comparison of effective oil-and-gaz-saturated pore volumes as to the section of each deposit of North near-edge zone of Dnieper-Donetsk depression a baseline horizon has been defined. The baseline horizon is characterized by most effective oil-and-gaz-saturation of pores volume. The features of fluid zoning for each field were identified relative to their base horizons. As the result three types of vertical zoning fluid deposits were identified. First - horizons with less oil-and-gaz-saturation pore volumes of the section lie below and above of the base horizon, second – lie below the base of the horizon; third - above the base horizon. According to the established zoning fluid typing the forecast of new horizons and underexplored areas within opened fields of Dnieper-Donetsk depression were made. In the second type of multilayer fields perspective horizons and underexplored areas were forecasted below the baseline horizons. In the third type of multilayer fields are forecasted above baseline horizons.

Author Biographies

В. М. Абєлєнцев, Ukrainian Research Institute for Natural Gases

PhD (Geology), Head of Department

А. Й. Лур’є, V.N. Karazin Kharkiv National University

Doctor of Sciences (Geology and Mineralogy), Full Professor

Л. O. Міщенко, Ukrainian Research Institute for Natural Gases

Senior Researcher

References

Abyelyentsev, V. M., Lur"ye, A. Y., Mishchenko, L. O. (2014). Heolohichni umovy vyluchennya zalyshkovykh zapasiv i dorozvidky rodovyshch vuhlevodniv pivnichnoyi prybortovoyi zony Dniprovs'ko-Donets'koyi zapadyny. Monohrafiya, Kh. KhNU imeni V. N. Karazina, 192, ISBN 978-966-285-098-7.

Abyelyentsev, V.M. (2004). Shchodo prychyn zarodzhennya ta diyi mekhanizmu vybirkovoho obvodnennya hazokondensatnykh pokladiv. Zb. nauk. pr. Pytannya rozv. hazovoyi prom-ti Ukrayiny, UkrNDIhaz., Vyp. 37. Kharkiv, 199-202.

Abyelyentsev, V.M., Lur"ye, A.Y., Nesterenko, M.Yu. (2013). Osoblyvosti obvodnennya hazokondensatnykh ta naftovykh pokladiv rodovyshch Dniprovs'ko-Donets'koyi zapadyny. zb. Visnyk KhNU imeni V. N. Karazina. Kharkiv, 1084, 39, 9-14.

Lur"ye, A.Y., Abyelyentsev, V.M., Mishchenko, L.O. (2015). Heolohichni osoblyvosti bahatoplastovykh rodovyshch vuhlevodniv yak osnova vyznachennya kryteriyiv yikh dorozvidky. zb. Visnyk KhNU imeni V. N. Karazina. Kharkiv, 1157, 42, 27-31.

Abyelyentsev, V.M., Susyak, T.Ya. (2015). Umovy vynyknennya zashchemlenykh hazovykh skupchen' v protsesi vybirkovoho obvodnennya pokladiv. zb. Visnyk KhNU imeni V. N. Karazina. Kharkiv, 1157, 42, 7-11.

Abyelyentsev, V.M., Leshchenko, L.Z. (2010). Osoblyvosti vydobutku vuhlevodniv iz rodovyshch, yaki perebuvayut' na zavershal'niy stadiyi yikh rozrobky. zb. Visnyk KhNU imeni V. N. Karazina. Kharkiv, 924, 6-9.

Vysochans'kyy, I.V. (2015) Naukovi zasady poshukiv nesklepinnykh pastok vuhlevodniv u Dniprovs'ko-Donets'komu avlakoheni. Monohrafiya, Kh. KhNU imeni V. N. Karazina, 236, 978-966-285-195-3.

Dem"yanenko, I.I. (2004) Problemy i optymizatsiya naftohazoposhukovykh i rozviduval'nykh robit na ob"yektakh Dniprovs'ko-Donets'koyi zapadyny. Chernihiv. TsNTEI, 220, 966-7905-50-0.

Lynetskyi, V.F. (1965). Myhratsyia nefty y formyrovanye ee zalezhei. Kyev, Naukova dumka, 200.

Zavialov, V.M. (1973). Uslovyia akkumuliatsyy nefty y haza y zakonomernosty razmeshchenyia ykh v Dneprovsko-Donetskoi vpadyne. M., Nedra, 120.

Tereshchenko, V.A. (1977). Nekotorіe zakonomernosty razmeshchenyia zalezhei nefty y haza v sviazy so stadyiamy preobrazovanyia porod y heotemperaturnіmy uslovyiamy. Tezysі dokladov Respublykanskoho soveshchanyia. Lvov, 140–141.

Dolenko, H.N., Varychev, S. A., Kolodyi, V.V. y dr (1989). Razlomnaia tektonyka y neftehazonosnost Ukraynы. Kyev, Naukova dumka, 116.

Vіsochanskyi, Y.V., Krot, V.V., Chebanenko, Y.Y. y dr. (1990). Tektonycheskye narushenyia y voprosі neftehazonosnosty (osobennosty tektonyky Dneprovsko-Donbasskoho avlakohena). Kyev, YHN AN USSR, 38.

Arsyryy, Yu.A., Kholodnіkh, A.B., Stryzhak, V.P. (2002). K voprosu o stroenyy y tektonycheskom rayonyrovanyy prybortovikh zon Dneprovsko-Donetskoy vpadynы. Heolohycheskyy zhurnal, Kyev, 4, 33-41.

Kryvulya, S.V. (2014). Kryteriyi dorozvidky velykykh rodovyshch vuhlevodniv u nyzhn'operms'ko-verkhn'okam"yanovuhil'nykh vidkladakh Dniprovs'ko-Donets'koyi zapadyny. Monohrafiya, Kh. UkrNDIhaz, NTU «KhPI», 174, 978-966-2166-93-4.

Vysochanskyi, I.V. (1994). Struktury-pastky nafty i hazu plat formovykh rehioniv (na prykladi Dniprovsko-Donetskoi zapadyny). Dys. … d. heol.-miner. Nauk. u vyhliadi naukovoi dopovidi. Lviv, 61.

Myshchenko, L.A. Osobennosty poyskov zalezhey uhlevodorodov v neantyklynal'nіkh klynoformnіkh telakh Dneprovsko-Donetskoy vpadynі (2014) Neftehazovaya heolohyya. Teoryya y praktyka, 9, 2. Aviable at: http://www.ngtp.ru/rub/4/28_2014.pdf

Abyelyentsev, V.M., Lur"ye, A.Y., Mishchenko, L.O. (2014). Doslidzhennia neodnoridnosti porovoho seredovyshcha plastiv-kolektoriv z metoiu optymizatsii vyluchennia vuhlevodniv. zb. Visnyk KhNU imeni V. N. Karazina. Kharkiv, 1128, 41, 9-14.

Abyelyentsev, V.M. (2002). Otsinka dyferentsiatsiyi shchil'nosti zalyshkovykh zapasiv ta yikh ob"yemiv po ploshchi ta rozrizu pokladiv hazokondensatnoho horyzontu S-5 Zakhidno- ta Skhidno-Berezivs'koho rodovyshch. zb. “Pytannya rozvytku hazovoyi promyslovosti Ukrayiny”. Kharkiv, UkrNDIhaz, 30, 23-31.

Lurie, A.I., Abielientsev, V.M., Bikman, Ye.S., Mishchenko, L.O. (2004). Novi dani pro heolohichnu budovu ta hazonosnist verkhnovizeiskykh pokladiv Hadiatskoho rodovyshcha. zb. “Pytannia rozvytku hazovoi promyslovosti Ukrainy”. Kharkiv, UkrNDIhaz, 33, 10-12.

Published

2016-01-27

Issue

Section

Geology