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Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature. / Vorontsov, A. A.; Perfilova, O. Yu; Kruk, N. N. et al.

In: Doklady Earth Sciences, Vol. 485, No. 2, 01.04.2019, p. 347-354.

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

Harvard

Vorontsov, AA, Perfilova, OY, Kruk, NN & Tarasyuk, AS 2019, 'Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature', Doklady Earth Sciences, vol. 485, no. 2, pp. 347-354. https://doi.org/10.1134/S1028334X19040093

APA

Vorontsov, A. A., Perfilova, O. Y., Kruk, N. N., & Tarasyuk, A. S. (2019). Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature. Doklady Earth Sciences, 485(2), 347-354. https://doi.org/10.1134/S1028334X19040093

Vancouver

Vorontsov AA, Perfilova OY, Kruk NN, Tarasyuk AS. Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature. Doklady Earth Sciences. 2019 Apr 1;485(2):347-354. doi: 10.1134/S1028334X19040093

Author

Vorontsov, A. A. ; Perfilova, O. Yu ; Kruk, N. N. et al. / Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature. In: Doklady Earth Sciences. 2019 ; Vol. 485, No. 2. pp. 347-354.

BibTeX

@article{cf4eac0fac224974b3be454791652fa7,
title = "Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature",
abstract = "Abstract: The results of geological–geochemical studies of some Late Ordovician associations in the frame of the Minusinsk Trough with available geological and U–Pb, Rb–Sr, and K–Ar age dates are presented. The Late Ordovician volcanic rocks form a continuous igneous series, the basalts of which are different from Devonian basalts of the Minusinsk Trough in the lower TiO2 content (≥ 1.7 wt %) and more fractionated REE pattern. These features should be considered the index characteristics of Late Ordovician rocks. Their compositions reflect processes of fractionation crystallization and mixing of trachibasaltic magmas with crustal melts. When taking into account the regional geological data, it is shown that magmatic activity at the Late Ordovician endogenic evolution stage in the northern part of the Altai–Sayan fold area was caused by the interaction of a mantle plume and the lithospheric mantle, which was metasomatically reworked and enriched in water during former subduction processes.",
keywords = "MANTLE PLUMES",
author = "Vorontsov, {A. A.} and Perfilova, {O. Yu} and Kruk, {N. N.} and Tarasyuk, {A. S.}",
note = "Publisher Copyright: {\textcopyright} 2019, Pleiades Publishing, Ltd.",
year = "2019",
month = apr,
day = "1",
doi = "10.1134/S1028334X19040093",
language = "English",
volume = "485",
pages = "347--354",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Late Ordovician Volcanism of the Northern Part of Altai–Sayan Area and Its Geodynamic Nature

AU - Vorontsov, A. A.

AU - Perfilova, O. Yu

AU - Kruk, N. N.

AU - Tarasyuk, A. S.

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

PY - 2019/4/1

Y1 - 2019/4/1

N2 - Abstract: The results of geological–geochemical studies of some Late Ordovician associations in the frame of the Minusinsk Trough with available geological and U–Pb, Rb–Sr, and K–Ar age dates are presented. The Late Ordovician volcanic rocks form a continuous igneous series, the basalts of which are different from Devonian basalts of the Minusinsk Trough in the lower TiO2 content (≥ 1.7 wt %) and more fractionated REE pattern. These features should be considered the index characteristics of Late Ordovician rocks. Their compositions reflect processes of fractionation crystallization and mixing of trachibasaltic magmas with crustal melts. When taking into account the regional geological data, it is shown that magmatic activity at the Late Ordovician endogenic evolution stage in the northern part of the Altai–Sayan fold area was caused by the interaction of a mantle plume and the lithospheric mantle, which was metasomatically reworked and enriched in water during former subduction processes.

AB - Abstract: The results of geological–geochemical studies of some Late Ordovician associations in the frame of the Minusinsk Trough with available geological and U–Pb, Rb–Sr, and K–Ar age dates are presented. The Late Ordovician volcanic rocks form a continuous igneous series, the basalts of which are different from Devonian basalts of the Minusinsk Trough in the lower TiO2 content (≥ 1.7 wt %) and more fractionated REE pattern. These features should be considered the index characteristics of Late Ordovician rocks. Their compositions reflect processes of fractionation crystallization and mixing of trachibasaltic magmas with crustal melts. When taking into account the regional geological data, it is shown that magmatic activity at the Late Ordovician endogenic evolution stage in the northern part of the Altai–Sayan fold area was caused by the interaction of a mantle plume and the lithospheric mantle, which was metasomatically reworked and enriched in water during former subduction processes.

KW - MANTLE PLUMES

UR - http://www.scopus.com/inward/record.url?scp=85066932101&partnerID=8YFLogxK

U2 - 10.1134/S1028334X19040093

DO - 10.1134/S1028334X19040093

M3 - Article

AN - SCOPUS:85066932101

VL - 485

SP - 347

EP - 354

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 20532039