Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
A-Type Granite Formation in the Yenisei Ridge in the Cryogenian Period during the Tectonic Transformation of the Region (Southwestern Framing of the Siberian Craton). / Vernikovskaya, A. E.; Vernikovsky, V. A.; Matushkin, N. Yu и др.
в: Doklady Earth Sciences, Том 507, 2022, стр. S269-S277.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - A-Type Granite Formation in the Yenisei Ridge in the Cryogenian Period during the Tectonic Transformation of the Region (Southwestern Framing of the Siberian Craton)
AU - Vernikovskaya, A. E.
AU - Vernikovsky, V. A.
AU - Matushkin, N. Yu
AU - Wingate, M. T.D.
AU - Romanova, I. V.
AU - Kadilnikov, P. I.
AU - Bogdanov, E. A.
N1 - Публикация для корректировки.
PY - 2022
Y1 - 2022
N2 - We consider the evolution of A-type granite magmatism in the Cryogenian period during a tectonic transition of the Yenisei Ridge from its postcollisional state to the early development stages of an active continental margin. New geochronological and geochemical data are reported for A-type granites of two intrusions – the Strelka pluton belonging to the postcollisional Glushikha complex (752–718 Ma) and the Yagodka pluton of the Tatarka complex that formed on the active continental margin (711–629 Ma). New U–Pb and Ar/Ar geochronological data for these intrusions indicate that the time intervals for these two complexes overlap, showing the unbroken evolution of A-type magmatism during the tectonic transformation of the region.
AB - We consider the evolution of A-type granite magmatism in the Cryogenian period during a tectonic transition of the Yenisei Ridge from its postcollisional state to the early development stages of an active continental margin. New geochronological and geochemical data are reported for A-type granites of two intrusions – the Strelka pluton belonging to the postcollisional Glushikha complex (752–718 Ma) and the Yagodka pluton of the Tatarka complex that formed on the active continental margin (711–629 Ma). New U–Pb and Ar/Ar geochronological data for these intrusions indicate that the time intervals for these two complexes overlap, showing the unbroken evolution of A-type magmatism during the tectonic transformation of the region.
KW - A-type granite
KW - Ar/Ar
KW - Cryogenian
KW - U–Pb
KW - Yenisei Ridge
KW - geochemistry
KW - geochronology
UR - https://www.mendeley.com/catalogue/253cdc39-eb8f-330c-8885-a2ae85adec81/
U2 - 10.1134/S1028334X22601183
DO - 10.1134/S1028334X22601183
M3 - Article
VL - 507
SP - S269-S277
JO - Doklady Earth Sciences
JF - Doklady Earth Sciences
SN - 1028-334X
ER -
ID: 55694769