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Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement. / Simonov, V. A.; Kontorovich, V. A.; Stupakov, S. I. et al.

In: Doklady Earth Sciences, Vol. 486, No. 2, 01.06.2019, p. 613-616.

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

Harvard

Simonov, VA, Kontorovich, VA, Stupakov, SI, Filippov, YF, Saraev, SV & Kotlyarov, AV 2019, 'Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement', Doklady Earth Sciences, vol. 486, no. 2, pp. 613-616. https://doi.org/10.1134/S1028334X19060217

APA

Simonov, V. A., Kontorovich, V. A., Stupakov, S. I., Filippov, Y. F., Saraev, S. V., & Kotlyarov, A. V. (2019). Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement. Doklady Earth Sciences, 486(2), 613-616. https://doi.org/10.1134/S1028334X19060217

Vancouver

Simonov VA, Kontorovich VA, Stupakov SI, Filippov YF, Saraev SV, Kotlyarov AV. Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement. Doklady Earth Sciences. 2019 Jun 1;486(2):613-616. doi: 10.1134/S1028334X19060217

Author

Simonov, V. A. ; Kontorovich, V. A. ; Stupakov, S. I. et al. / Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement. In: Doklady Earth Sciences. 2019 ; Vol. 486, No. 2. pp. 613-616.

BibTeX

@article{2f0262cd22144049bb7e624f4f478b40,
title = "Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement",
abstract = "40Ar/39Ar analysis showed a simultaneous (at about 490 Ma) formation of the Paleozoic picrite and basalt complexes of the West Siberian Plate basement. The petrochemistry, trace and REE geochemistry, and composition of clinopyroxene indicate the formation of the picrite of well no. 11 (Chkalov area) as a result of intraplate magmatism of the OIB type. Calculations based on the compositions of clinopyroxene allowed crystallization of minerals of porphyric picrite at 1215–1275°C and 4.5–8 kbar. In general, it has been found that the picrite basalt complexes considered were formed from enriched igneous plume systems under intraplate conditions near the active margin of the ancient ocean.",
author = "Simonov, {V. A.} and Kontorovich, {V. A.} and Stupakov, {S. I.} and Filippov, {Yu F.} and Saraev, {S. V.} and Kotlyarov, {A. V.}",
note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd.",
year = "2019",
month = jun,
day = "1",
doi = "10.1134/S1028334X19060217",
language = "English",
volume = "486",
pages = "613--616",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Setting of the Formation of Paleozoic Picrite Basalt Complexes in the West Siberian Plate Basement

AU - Simonov, V. A.

AU - Kontorovich, V. A.

AU - Stupakov, S. I.

AU - Filippov, Yu F.

AU - Saraev, S. V.

AU - Kotlyarov, A. V.

N1 - Publisher Copyright: © 2019, Pleiades Publishing, Ltd.

PY - 2019/6/1

Y1 - 2019/6/1

N2 - 40Ar/39Ar analysis showed a simultaneous (at about 490 Ma) formation of the Paleozoic picrite and basalt complexes of the West Siberian Plate basement. The petrochemistry, trace and REE geochemistry, and composition of clinopyroxene indicate the formation of the picrite of well no. 11 (Chkalov area) as a result of intraplate magmatism of the OIB type. Calculations based on the compositions of clinopyroxene allowed crystallization of minerals of porphyric picrite at 1215–1275°C and 4.5–8 kbar. In general, it has been found that the picrite basalt complexes considered were formed from enriched igneous plume systems under intraplate conditions near the active margin of the ancient ocean.

AB - 40Ar/39Ar analysis showed a simultaneous (at about 490 Ma) formation of the Paleozoic picrite and basalt complexes of the West Siberian Plate basement. The petrochemistry, trace and REE geochemistry, and composition of clinopyroxene indicate the formation of the picrite of well no. 11 (Chkalov area) as a result of intraplate magmatism of the OIB type. Calculations based on the compositions of clinopyroxene allowed crystallization of minerals of porphyric picrite at 1215–1275°C and 4.5–8 kbar. In general, it has been found that the picrite basalt complexes considered were formed from enriched igneous plume systems under intraplate conditions near the active margin of the ancient ocean.

UR - http://www.scopus.com/inward/record.url?scp=85070218798&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19060217

DO - 10.1134/S1028334X19060217

M3 - Article

AN - SCOPUS:85070218798

VL - 486

SP - 613

EP - 616

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 25705780