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Artyushkov, E. V., Chekhovich, P. A. (2024) Crustal Subsidence in the West Siberian Sedimentary Basin Caused by Prograde Metamorphism-Induced Rock Contraction in the Lower Crust. Doklady Earth Sciences, 515 (2) 743-755 doi:10.1134/s1028334x23603711

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Reference TypeJournal (article/letter/editorial)
TitleCrustal Subsidence in the West Siberian Sedimentary Basin Caused by Prograde Metamorphism-Induced Rock Contraction in the Lower Crust
JournalDoklady Earth Sciences
AuthorsArtyushkov, E. V.Author
Chekhovich, P. A.Author
Year2024 (April)Volume515
Issue2
PublisherPleiades Publishing Ltd
DOIdoi:10.1134/s1028334x23603711Search in ResearchGate
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Mindat Ref. ID17389732Long-form Identifiermindat:1:5:17389732:6
GUID0
Full ReferenceArtyushkov, E. V., Chekhovich, P. A. (2024) Crustal Subsidence in the West Siberian Sedimentary Basin Caused by Prograde Metamorphism-Induced Rock Contraction in the Lower Crust. Doklady Earth Sciences, 515 (2) 743-755 doi:10.1134/s1028334x23603711
Plain TextArtyushkov, E. V., Chekhovich, P. A. (2024) Crustal Subsidence in the West Siberian Sedimentary Basin Caused by Prograde Metamorphism-Induced Rock Contraction in the Lower Crust. Doklady Earth Sciences, 515 (2) 743-755 doi:10.1134/s1028334x23603711
In(2024, April) Doklady Earth Sciences Vol. 515 (2) Pleiades Publishing Ltd

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Artyushkov, E. V., Chekhovich, P. A. (2025) The West Siberian Sedimentary Basin. Highly Heterogeneous Crustal Subsidence: A Result of Metamorphism Catalyzed by an Influx of Mantle Fluids. Doklady Earth Sciences, 520 (1). doi:10.1134/s1028334x24604140
Artyushkov, E. V., Chekhovich, P. A. (2014) Neotectonic uplift of Early Precambrian cratons caused by metamorphism with rock expansion in the earth crust. Doklady Earth Sciences, 458 (2) 1215-1219 doi:10.1134/s1028334x14100158
Artyushkov, E. V., Chekhovich, P. A. (2023) The Origin of the West Siberian Sedimentary Basin without Strong Crustal Stretching: An Analysis of Superdeep Drilling Data. Doklady Earth Sciences, 512 (2) 1006-1013 doi:10.1134/s1028334x23601517
Artyushkov, E. V., Chekhovich, P. A. (2024) Erratum to: The Origin of the West Siberian Sedimentary Basin without Strong Crustal Stretching: An Analysis of Superdeep Drilling Data. Doklady Earth Sciences, 514 (1) 212 doi:10.1134/s1028334x23070371
Artyushkov, E. V., Belyaev, I. V., Kazanin, G. S., Pavlov, S. P., Chekhovich, P. A., Shkarubo, S. I. (2013) The formation of ultradeep sedimentary basins through metamorphism with rock contraction in continental crust. Doklady Earth Sciences, 452 (2) 988-991 doi:10.1134/s1028334x13100085
Artyushkov, E. V., Chekhovich, P. A. (2022) The Role of Deep Fluids in Crustal Subsidence of the Cratonic Interior: The Moscow Sedimentary Basin during the Late Devonian. Doklady Earth Sciences, 507 (2) 1085-1095 doi:10.1134/s1028334x22601018
Artyushkov, E. V., Kanygin, A. V., Tesakov, Yu. I., Chekhovich, P. A. (2007) Sea level in the Ordovician: Sharp fluctuations in subsidence rates of the Siberian Craton crust. Doklady Earth Sciences, 412 (1) 53-57 doi:10.1134/s1028334x07010126
Artyushkov, E. V., Korikovsky, S. P., Massonne, H. -J., Chekhovich, P. A. (2018) Petrological Data Allow Estimating the Amplitudes of Crustal Uplifts Caused by Retrograde Metamorphism. Doklady Earth Sciences, 482 (1) 1125-1129 doi:10.1134/s1028334x18090015
Artyushkov, E. V., Smirnov, O. E., Chekhovich, P. A. (2021) The Deep Submerged Continental Crust: The Central Arctic and Zealandia in the Southwest Pacific. Doklady Earth Sciences, 501 (2) 1043-1048 doi:10.1134/s1028334x21120023
Artyushkov, E. V., Chekhovich, P. A. (2022) Non-Uniform Crustal Subsidence due to the Infiltration of Mantle Fluids: A Case Study of the Moscow Syneclise during the Middle Devonian. Doklady Earth Sciences, 505 (1) 471-482 doi:10.1134/s1028334x22070030
Artyushkov, E. V., Kol’ka, V. V., Chekhovich, P. A. (2020) The Occurrence of a Lower Viscosity Layer in the Crust of Old Cratons as a Cause of the Strongly Differentiated Character of Postglacial Uplift. Doklady Earth Sciences, 492 (1). 351-355 doi:10.1134/s1028334x20050037
 
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