Standard

Plume magmatism in the northeastern part of the Altai–Sayan region : Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression). / Vorontsov, A. A.; Perfilova, O. Yu; Buslov, M. M. и др.

в: Doklady Earth Sciences, Том 472, № 2, 01.02.2017, стр. 184-189.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Vorontsov, AA, Perfilova, OY, Buslov, MM, Travin, AV, Makhlaev, ML, Dril, SI & Katraevskaya, YI 2017, 'Plume magmatism in the northeastern part of the Altai–Sayan region: Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression)', Doklady Earth Sciences, Том. 472, № 2, стр. 184-189. https://doi.org/10.1134/S1028334X1702009X

APA

Vorontsov, A. A., Perfilova, O. Y., Buslov, M. M., Travin, A. V., Makhlaev, M. L., Dril, S. I., & Katraevskaya, Y. I. (2017). Plume magmatism in the northeastern part of the Altai–Sayan region: Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression). Doklady Earth Sciences, 472(2), 184-189. https://doi.org/10.1134/S1028334X1702009X

Vancouver

Vorontsov AA, Perfilova OY, Buslov MM, Travin AV, Makhlaev ML, Dril SI и др. Plume magmatism in the northeastern part of the Altai–Sayan region: Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression). Doklady Earth Sciences. 2017 февр. 1;472(2):184-189. doi: 10.1134/S1028334X1702009X

Author

Vorontsov, A. A. ; Perfilova, O. Yu ; Buslov, M. M. и др. / Plume magmatism in the northeastern part of the Altai–Sayan region : Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression). в: Doklady Earth Sciences. 2017 ; Том 472, № 2. стр. 184-189.

BibTeX

@article{09ea01a6da3c4775b4f4a59609e98e1e,
title = "Plume magmatism in the northeastern part of the Altai–Sayan region: Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression)",
abstract = "The results of geochronological (U–Pb, Ar–Ar), geochemical, and isotopic (Sr, Nd) studies of the Ordovician and Devonian mafic volcanic–subvolcanic rock associations of the Minusinsk Depression are presented. The obtained ages of magmatic associations and the basite composition, considering previous studies, witness to the impact of two mantle plumes different in age (Late Cambrian–Ordovician and Devonian) on suprasubduction rock complexes in active continental margin settings.",
author = "Vorontsov, {A. A.} and Perfilova, {O. Yu} and Buslov, {M. M.} and Travin, {A. V.} and Makhlaev, {M. L.} and Dril, {S. I.} and Katraevskaya, {Ya I.}",
year = "2017",
month = feb,
day = "1",
doi = "10.1134/S1028334X1702009X",
language = "English",
volume = "472",
pages = "184--189",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - Plume magmatism in the northeastern part of the Altai–Sayan region

T2 - Stages, source compositions, and geodynamics (exemplified by the Minusinsk Depression)

AU - Vorontsov, A. A.

AU - Perfilova, O. Yu

AU - Buslov, M. M.

AU - Travin, A. V.

AU - Makhlaev, M. L.

AU - Dril, S. I.

AU - Katraevskaya, Ya I.

PY - 2017/2/1

Y1 - 2017/2/1

N2 - The results of geochronological (U–Pb, Ar–Ar), geochemical, and isotopic (Sr, Nd) studies of the Ordovician and Devonian mafic volcanic–subvolcanic rock associations of the Minusinsk Depression are presented. The obtained ages of magmatic associations and the basite composition, considering previous studies, witness to the impact of two mantle plumes different in age (Late Cambrian–Ordovician and Devonian) on suprasubduction rock complexes in active continental margin settings.

AB - The results of geochronological (U–Pb, Ar–Ar), geochemical, and isotopic (Sr, Nd) studies of the Ordovician and Devonian mafic volcanic–subvolcanic rock associations of the Minusinsk Depression are presented. The obtained ages of magmatic associations and the basite composition, considering previous studies, witness to the impact of two mantle plumes different in age (Late Cambrian–Ordovician and Devonian) on suprasubduction rock complexes in active continental margin settings.

UR - http://www.scopus.com/inward/record.url?scp=85018491879&partnerID=8YFLogxK

U2 - 10.1134/S1028334X1702009X

DO - 10.1134/S1028334X1702009X

M3 - Article

AN - SCOPUS:85018491879

VL - 472

SP - 184

EP - 189

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 10263077