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History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin. / Pervukhina, N. V.; Shemin, G. G.; Moskvin, V. I.

In: Russian Geology and Geophysics, Vol. 58, No. 3-4, 01.04.2017, p. 384-392.

Research output: Contribution to journal › Article › peer-review

Harvard

Pervukhina, NV, Shemin, GG & Moskvin, VI 2017, 'History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin', Russian Geology and Geophysics, vol. 58, no. 3-4, pp. 384-392. https://doi.org/10.1016/j.rgg.2016.09.013

APA

Pervukhina, N. V., Shemin, G. G., & Moskvin, V. I. (2017). History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin. Russian Geology and Geophysics, 58(3-4), 384-392. https://doi.org/10.1016/j.rgg.2016.09.013

Vancouver

Pervukhina NV, Shemin GG, Moskvin VI. History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin. Russian Geology and Geophysics. 2017 Apr 1;58(3-4):384-392. doi: 10.1016/j.rgg.2016.09.013

Author

Pervukhina, N. V. ; Shemin, G. G. ; Moskvin, V. I. / History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin. In: Russian Geology and Geophysics. 2017 ; Vol. 58, No. 3-4. pp. 384-392.

BibTeX

@article{422cca3e233b44a4a6dc2cf1df46b2f2,
title = "History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin",
abstract = "The paper presents new paleotectonic data on the Bovanenkovo, Taz, and Gubkin dome-shaped uplifts and the Novyi Port, Urengoi, Kharampur, and Medvezh'e swells, with implications for the history of zone J2 and the Jurassic reservoir as a whole. Most of the large uplifts originated in the Early-Middle Jurassic and completed their evolution in the early Late Cretaceous (latest Cenomanian), generally (Bovanenkovo, Novyi Port, Kharampur, and Taz) or to a large extent (Urengoi and Gubkin), except for the much younger Medvezh'e swell, which formed in the Paleogene-Quaternary interval. The conditions for oil storage and retention in anticlinal traps of Jurassic zones J1 and J2 were the most favorable between the middle Late Cretaceous and the Eocene, inclusive. Gas accumulation lasted for a much longer time, from the Late Jurassic to the Present, and was especially rapid in the Late Cretaceous-Paleogene.",
keywords = "gas, oil, paleotectonic reconstructions, reservoir history, traps",
author = "Pervukhina, {N. V.} and Shemin, {G. G.} and Moskvin, {V. I.}",
year = "2017",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2016.09.013",
language = "English",
volume = "58",
pages = "384--392",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "3-4",

}

RIS

TY - JOUR

T1 - History of anticlinal traps and oil and gas fields in Jurassic reservoirs in the northern West Siberian basin

AU - Pervukhina, N. V.

AU - Shemin, G. G.

AU - Moskvin, V. I.

PY - 2017/4/1

Y1 - 2017/4/1

N2 - The paper presents new paleotectonic data on the Bovanenkovo, Taz, and Gubkin dome-shaped uplifts and the Novyi Port, Urengoi, Kharampur, and Medvezh'e swells, with implications for the history of zone J2 and the Jurassic reservoir as a whole. Most of the large uplifts originated in the Early-Middle Jurassic and completed their evolution in the early Late Cretaceous (latest Cenomanian), generally (Bovanenkovo, Novyi Port, Kharampur, and Taz) or to a large extent (Urengoi and Gubkin), except for the much younger Medvezh'e swell, which formed in the Paleogene-Quaternary interval. The conditions for oil storage and retention in anticlinal traps of Jurassic zones J1 and J2 were the most favorable between the middle Late Cretaceous and the Eocene, inclusive. Gas accumulation lasted for a much longer time, from the Late Jurassic to the Present, and was especially rapid in the Late Cretaceous-Paleogene.

AB - The paper presents new paleotectonic data on the Bovanenkovo, Taz, and Gubkin dome-shaped uplifts and the Novyi Port, Urengoi, Kharampur, and Medvezh'e swells, with implications for the history of zone J2 and the Jurassic reservoir as a whole. Most of the large uplifts originated in the Early-Middle Jurassic and completed their evolution in the early Late Cretaceous (latest Cenomanian), generally (Bovanenkovo, Novyi Port, Kharampur, and Taz) or to a large extent (Urengoi and Gubkin), except for the much younger Medvezh'e swell, which formed in the Paleogene-Quaternary interval. The conditions for oil storage and retention in anticlinal traps of Jurassic zones J1 and J2 were the most favorable between the middle Late Cretaceous and the Eocene, inclusive. Gas accumulation lasted for a much longer time, from the Late Jurassic to the Present, and was especially rapid in the Late Cretaceous-Paleogene.

KW - gas

KW - oil

KW - paleotectonic reconstructions

KW - reservoir history

KW - traps

UR - http://www.scopus.com/inward/record.url?scp=85018498406&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.09.013

DO - 10.1016/j.rgg.2016.09.013

M3 - Article

AN - SCOPUS:85018498406

VL - 58

SP - 384

EP - 392

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 3-4

ER -

ID: 10036152