Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton

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Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton. / Vernikovskaya, A. E.; Vernikovsky, V. A.; Matushkin, N. Yu и др.

в: Russian Geology and Geophysics, Том 64, № 6, 06.2023, стр. 647-668.

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

BibTeX

@article{3e87046a8be04114889be5fee8953630,

title = "Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton",

abstract = "We document the evolution of A-type granitoid magmatism during the Cryogenian tectonic transformation of the Yenisei Ridge from a postcollisional mode to the early stage of development of an active continental margin. We illustrate the A-type granitoid magmatism evolution in a model for the emplacement and cooling of the intrusions of the Strelka pluton, reflecting the final stage of magmatism during the formation of the postcollisional Glushikha complex (719–702 Ma). These processes took place at the same time as the formation of mantle, mantle-crustal and crustal rocks of the Tatarka complex (711–683 Ma), including the Yagodka pluton A-type granites (711–705 Ma) during the early stage of active continental margin development. During this period of tectonic transition, both convergent events involved the continuous formation of felsic intrusions corresponding to oxidized A-type granites.",

keywords = "A-type granites, Siberian Craton, U–Pb and40Ar/39Ar geochronology, Yenisei Ridge, active continental margin, collision",

author = "Vernikovskaya, {A. E.} and Vernikovsky, {V. A.} and Matushkin, {N. Yu} and Kadilnikov, {P. I.} and Wingate, {M. T.D.} and Bogdanov, {E. A.} and Travin, {A. V.}",

note = "This study was financially supported by the Russian Science Foundation (grant No. 22-27-00178).",

year = "2023",

month = jun,

doi = "10.2113/RGG20224532",

language = "English",

volume = "64",

pages = "647--668",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "6",

}

RIS

TY - JOUR

T1 - Cryogenian A-type Granites of the Yenisei Ridge – Indicators of Tectonic Transformation in the Southwestern Margin of the Siberian Craton

AU - Vernikovskaya, A. E.

AU - Vernikovsky, V. A.

AU - Matushkin, N. Yu

AU - Kadilnikov, P. I.

AU - Wingate, M. T.D.

AU - Bogdanov, E. A.

AU - Travin, A. V.

N1 - This study was financially supported by the Russian Science Foundation (grant No. 22-27-00178).

PY - 2023/6

Y1 - 2023/6

N2 - We document the evolution of A-type granitoid magmatism during the Cryogenian tectonic transformation of the Yenisei Ridge from a postcollisional mode to the early stage of development of an active continental margin. We illustrate the A-type granitoid magmatism evolution in a model for the emplacement and cooling of the intrusions of the Strelka pluton, reflecting the final stage of magmatism during the formation of the postcollisional Glushikha complex (719–702 Ma). These processes took place at the same time as the formation of mantle, mantle-crustal and crustal rocks of the Tatarka complex (711–683 Ma), including the Yagodka pluton A-type granites (711–705 Ma) during the early stage of active continental margin development. During this period of tectonic transition, both convergent events involved the continuous formation of felsic intrusions corresponding to oxidized A-type granites.

AB - We document the evolution of A-type granitoid magmatism during the Cryogenian tectonic transformation of the Yenisei Ridge from a postcollisional mode to the early stage of development of an active continental margin. We illustrate the A-type granitoid magmatism evolution in a model for the emplacement and cooling of the intrusions of the Strelka pluton, reflecting the final stage of magmatism during the formation of the postcollisional Glushikha complex (719–702 Ma). These processes took place at the same time as the formation of mantle, mantle-crustal and crustal rocks of the Tatarka complex (711–683 Ma), including the Yagodka pluton A-type granites (711–705 Ma) during the early stage of active continental margin development. During this period of tectonic transition, both convergent events involved the continuous formation of felsic intrusions corresponding to oxidized A-type granites.

KW - A-type granites

KW - Siberian Craton

KW - U–Pb and40Ar/39Ar geochronology

KW - Yenisei Ridge

KW - active continental margin

KW - collision

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85168125672&origin=inward&txGid=c589f8e4bc008a4b938ef33e2c2f98e7

UR - https://www.mendeley.com/catalogue/7f6c8e06-6c92-396c-9c99-894de3d65097/

U2 - 10.2113/RGG20224532

DO - 10.2113/RGG20224532

M3 - Article

VL - 64

SP - 647

EP - 668

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 6

ER -

ID: 55589671