INTERNAL STRUCTURES OF FAULT ZONES IN THE PRIOLKHONIE AND EVOLUTION OF THE STATE OF STRESSES OF THE UPPER CRUST OF THE BAIKAL RIFT

INTERNAL STRUCTURES OF FAULT ZONES IN THE PRIOLKHONIE AND EVOLUTION OF THE STATE OF STRESSES OF THE UPPER CRUST OF THE BAIKAL RIFT

The Priolkhonie is a tectonic block located in the central part of the Baikalsky Ridge; it was shifted in the Cenozoic, yet remains above the water level of Lake Baikal. In view of its unique positioning and abundant rock outcropped sites, especially at shorelines, we conducted studies of internal s...

Full description

Bibliographic Details
Main Author: Alexander V. Cheremnykh
Format: Article
Language:English
Published: Institute of the Earth's crust, Siberian Branch of RAS 2015-09-01
Series:Geodinamika i Tektonofizika
Subjects:
baikal rift
fault zones
state of stresses
tectonic fracturing
Online Access:https://www.gt-crust.ru/jour/article/view/112

Similar Items

Similar Items