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

被引：3
|
作者：
Vernikovskaya, A. E. [1 ,2 ]
Vernikovsky, V. A. [1 ,2 ]
Matushkin, N. Yu. [1 ,2 ]
Kadilnikov, P. I. [1 ,2 ]
Wingate, M. T. D. [3 ]
Bogdanov, E. A. [1 ,2 ]
Travin, A. V. [4 ]
机构：
[1] Novosibirsk State Univ, Ul Pirogova 1, Novosibirsk 630090, Russia
[2] Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia
[3] Univ Western Australia, Sch Earth Sci, 35 Stirling Highway, Perth, WA 6009, Australia
[4] Russian Acad Sci, VS Sobolev Inst Geol & Mineral, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia
来源：
RUSSIAN GEOLOGY AND GEOPHYSICS | 2023年 / 64卷 / 06期
关键词：
A-type granites; collision; active continental margin; U-Pb and Ar-40; Ar-39; geochronology; Yenisei Ridge; Siberian Craton; WESTERN MARGIN; ALKALINE MAGMATISM; ZIRCON; EVOLUTION; PB; CLASSIFICATION; GEOCHRONOLOGY; ACCRETIONARY; REGION; OROGEN;
D O I：
10.2113/RGG20224532
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
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.
引用
收藏
页码：647 / 668
页数：22
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