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Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea. / Nikishin, A. M.; Gabdullin, R. R.; Makhatadze, G. V.; Khudolei, A. K.; Rubtsova, E. V.

в: Moscow University Geology Bulletin, Том 72, № 1, 01.01.2017, стр. 18-27.

Результаты исследований: Научные публикации в периодических изданияхстатьяРецензирование

Harvard

Nikishin, AM, Gabdullin, RR, Makhatadze, GV, Khudolei, AK & Rubtsova, EV 2017, 'Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea', Moscow University Geology Bulletin, Том. 72, № 1, стр. 18-27. https://doi.org/10.3103/S0145875217010082

APA

Nikishin, A. M., Gabdullin, R. R., Makhatadze, G. V., Khudolei, A. K., & Rubtsova, E. V. (2017). Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea. Moscow University Geology Bulletin, 72(1), 18-27. https://doi.org/10.3103/S0145875217010082

Vancouver

Nikishin AM, Gabdullin RR, Makhatadze GV, Khudolei AK, Rubtsova EV. Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea. Moscow University Geology Bulletin. 2017 Янв. 1;72(1):18-27. https://doi.org/10.3103/S0145875217010082

Author

Nikishin, A. M. ; Gabdullin, R. R. ; Makhatadze, G. V. ; Khudolei, A. K. ; Rubtsova, E. V. / Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea. в: Moscow University Geology Bulletin. 2017 ; Том 72, № 1. стр. 18-27.

BibTeX

@article{17b3e7aae5634d9b803f76cb42338146,
title = "Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea",
abstract = "The Bitak Formation is located in Crimea in the area of the city of Simferopol. It is mainly represented by weakly sorted conglomerates. The lithological description of the conglomerates is given. New data on the age of detrital zircons are presented. The possible age of the Bitak Formation is discussed. It is shown that the Bitak Formation is older than Late Bajocian volcanic rocks and younger than deposits of the Tauric Formation and its analogs of the same age. The Bitak Formation was accumulated in a pull-apart basin. Several basins of such a type are found in Crimea. It is thought that the Bitak basin was located at the base of the Middle Jurassic island-arc complex of Crimea.",
keywords = "Bitak conglomerates, Crimea, geological history, Jurassic",
author = "Nikishin, {A. M.} and Gabdullin, {R. R.} and Makhatadze, {G. V.} and Khudolei, {A. K.} and Rubtsova, {E. V.}",
year = "2017",
month = jan,
day = "1",
doi = "10.3103/S0145875217010082",
language = "English",
volume = "72",
pages = "18--27",
journal = "Moscow University Geology Bulletin",
issn = "0145-8752",
publisher = "Springer Nature",
number = "1",

}

RIS

TY - JOUR

T1 - Bitak conglomerates as a clue for understanding the Middle Jurassic geological history of Crimea

AU - Nikishin, A. M.

AU - Gabdullin, R. R.

AU - Makhatadze, G. V.

AU - Khudolei, A. K.

AU - Rubtsova, E. V.

PY - 2017/1/1

Y1 - 2017/1/1

N2 - The Bitak Formation is located in Crimea in the area of the city of Simferopol. It is mainly represented by weakly sorted conglomerates. The lithological description of the conglomerates is given. New data on the age of detrital zircons are presented. The possible age of the Bitak Formation is discussed. It is shown that the Bitak Formation is older than Late Bajocian volcanic rocks and younger than deposits of the Tauric Formation and its analogs of the same age. The Bitak Formation was accumulated in a pull-apart basin. Several basins of such a type are found in Crimea. It is thought that the Bitak basin was located at the base of the Middle Jurassic island-arc complex of Crimea.

AB - The Bitak Formation is located in Crimea in the area of the city of Simferopol. It is mainly represented by weakly sorted conglomerates. The lithological description of the conglomerates is given. New data on the age of detrital zircons are presented. The possible age of the Bitak Formation is discussed. It is shown that the Bitak Formation is older than Late Bajocian volcanic rocks and younger than deposits of the Tauric Formation and its analogs of the same age. The Bitak Formation was accumulated in a pull-apart basin. Several basins of such a type are found in Crimea. It is thought that the Bitak basin was located at the base of the Middle Jurassic island-arc complex of Crimea.

KW - Bitak conglomerates

KW - Crimea

KW - geological history

KW - Jurassic

UR - http://www.scopus.com/inward/record.url?scp=85020443920&partnerID=8YFLogxK

U2 - 10.3103/S0145875217010082

DO - 10.3103/S0145875217010082

M3 - Article

AN - SCOPUS:85020443920

VL - 72

SP - 18

EP - 27

JO - Moscow University Geology Bulletin

JF - Moscow University Geology Bulletin

SN - 0145-8752

IS - 1

ER -

ID: 62001847