THERMOCHRONOLOGY OF MINGLING DYKES IN WEST SANGILEN (SOUTH‐EAST TUVA, RUSSIA): EVIDENCE OF THE COLLAPSE OF THE COLLISIONAL SYSTEM IN THE NORTH‐WESTERN EDGE OF THE TUVA‐MONGOLIA MASSIF

THERMOCHRONOLOGY OF MINGLING DYKES IN WEST SANGILEN (SOUTH‐EAST TUVA, RUSSIA): EVIDENCE OF THE COLLAPSE OF THE COLLISIONAL SYSTEM IN THE NORTH‐WESTERN EDGE OF THE TUVA‐MONGOLIA MASSIF

In West Sangilen (South‐East Tuva, Russia), there are outcrops of metamorphic and magmatic complexes of early Caledonides, which are related to the period of long‐term collisional and post‐collisional events in the north‐ western edge of the Tuva‐Mongolian massif. The evolution of orogenic structure...

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Bibliographic Details
Main Authors: A. G. Vladimirov, I. V. Karmysheva, V. A. Yakovlev, A. V. Travin, A. A. Tsygankov, G. N. Burmakina
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2017-06-01
Series:Геодинамика и тектонофизика
Subjects:
thermochronology
mingling
collision
strike‐slip extension
tectonic denudation
sangilen
tuva‐mongolia massif
central asian folded belt
Online Access:https://www.gt-crust.ru/jour/article/view/363
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