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The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean. / Gordienko, I. V.; Metelkin, D. V.

In: Russian Geology and Geophysics, Vol. 57, No. 1, 01.01.2016, p. 69-81.

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

Harvard

Gordienko, IV & Metelkin, DV 2016, 'The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean', Russian Geology and Geophysics, vol. 57, no. 1, pp. 69-81. https://doi.org/10.1016/j.rgg.2016.01.005

APA

Gordienko, I. V., & Metelkin, D. V. (2016). The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean. Russian Geology and Geophysics, 57(1), 69-81. https://doi.org/10.1016/j.rgg.2016.01.005

Vancouver

Gordienko IV, Metelkin DV. The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean. Russian Geology and Geophysics. 2016 Jan 1;57(1):69-81. doi: 10.1016/j.rgg.2016.01.005

Author

Gordienko, I. V. ; Metelkin, D. V. / The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean. In: Russian Geology and Geophysics. 2016 ; Vol. 57, No. 1. pp. 69-81.

BibTeX

@article{5d81668c8c8a42aaae539779ad8cff38,
title = "The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean",
abstract = "The geodynamic reconstruction using new data on the composition, age, and paleomagnetism of Neoproterozoic and Vendian-Early Paleozoic island arc complexes has provided new insights into the evolution of the subduction zone magmatism over extensive areas of the Central Asian Orogenic Belt, including eastern Altai-Sayan, Transbaikalia, and Northern Mongolia. Comparison of the igneous complexes of modern and ancient ensimatic and ensialic island arcs in the subduction zone forms a basis for possible geodynamic scenarios of the subduction zone magmatism in Neoproterozoic and Vendian-Early Paleozoic island arcs in the zone of interaction between the Siberian paleocontinent and the Paleoasian Ocean, which take into account the composition of crustal and mantle (including mantle plume) components.",
keywords = "Early Paleozoic, Geodynamic reconstructions, Island arcs, Isotope age, Neoproterozoic, Paleoasian Ocean, Paleomagnetism, Petrological and geochemical composition, Siberian continent, Subduction zone magmatism",
author = "Gordienko, {I. V.} and Metelkin, {D. V.}",
year = "2016",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2016.01.005",
language = "English",
volume = "57",
pages = "69--81",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1",

}

RIS

TY - JOUR

T1 - The evolution of the subduction zone magmatism on the Neoproterozoic and Early Paleozoic active margins of the Paleoasian Ocean

AU - Gordienko, I. V.

AU - Metelkin, D. V.

PY - 2016/1/1

Y1 - 2016/1/1

N2 - The geodynamic reconstruction using new data on the composition, age, and paleomagnetism of Neoproterozoic and Vendian-Early Paleozoic island arc complexes has provided new insights into the evolution of the subduction zone magmatism over extensive areas of the Central Asian Orogenic Belt, including eastern Altai-Sayan, Transbaikalia, and Northern Mongolia. Comparison of the igneous complexes of modern and ancient ensimatic and ensialic island arcs in the subduction zone forms a basis for possible geodynamic scenarios of the subduction zone magmatism in Neoproterozoic and Vendian-Early Paleozoic island arcs in the zone of interaction between the Siberian paleocontinent and the Paleoasian Ocean, which take into account the composition of crustal and mantle (including mantle plume) components.

AB - The geodynamic reconstruction using new data on the composition, age, and paleomagnetism of Neoproterozoic and Vendian-Early Paleozoic island arc complexes has provided new insights into the evolution of the subduction zone magmatism over extensive areas of the Central Asian Orogenic Belt, including eastern Altai-Sayan, Transbaikalia, and Northern Mongolia. Comparison of the igneous complexes of modern and ancient ensimatic and ensialic island arcs in the subduction zone forms a basis for possible geodynamic scenarios of the subduction zone magmatism in Neoproterozoic and Vendian-Early Paleozoic island arcs in the zone of interaction between the Siberian paleocontinent and the Paleoasian Ocean, which take into account the composition of crustal and mantle (including mantle plume) components.

KW - Early Paleozoic

KW - Geodynamic reconstructions

KW - Island arcs

KW - Isotope age

KW - Neoproterozoic

KW - Paleoasian Ocean

KW - Paleomagnetism

KW - Petrological and geochemical composition

KW - Siberian continent

KW - Subduction zone magmatism

UR - http://www.scopus.com/inward/record.url?scp=84958674122&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2016.01.005

DO - 10.1016/j.rgg.2016.01.005

M3 - Article

AN - SCOPUS:84958674122

VL - 57

SP - 69

EP - 81

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1

ER -

ID: 25709122