Deep structure of the Salair fold-nappe terrane (NW CAOB) according to magnetotelluric sounding

Deep structure of the Salair fold-nappe terrane (NW CAOB) according to magnetotelluric sounding

The Salair fold-nappe terrane (a.k.a. Salair orogen, Salair) is the northwestern part of the Altai-Sayan folded area of the Central Asian Orogenic Belt. It is composed of Cambrian – Early Ordovician volcanic rocks and island-arc sedimentary deposits. In plan, Salair is a horseshoe-shaped structure w...

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Bibliographic Details
Main Authors: F. I. Zhimulev, E. V. Pospeeva, I. S. Novikov, V. V. Potapov
Format: Article
Language:English
Published: Institute of the Earth's crust, Siberian Branch of RAS 2021-03-01
Series:Geodinamika i Tektonofizika
Subjects:
magnetotelluric sounding
electrical conductivity anomaly
crust conductors
altai-sayan folded area
salair
tectonic nappes
orogeny
Online Access:https://www.gt-crust.ru/jour/article/view/1169

Internet

https://www.gt-crust.ru/jour/article/view/1169

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