THE ROLE OF GRAVITY IN FORMATION OF DEEP STRUCTURE  OF SHEAR ZONES

THE ROLE OF GRAVITY IN FORMATION OF DEEP STRUCTURE  OF SHEAR ZONES

Deformation structures which occur in rock masses in horizontal shear zones are studied with application of theoretical tectonophysical methods of analysis, including mathematical simulation of stresses. The paper presents results of such studies for cases with the rheology of geomedium represented...

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Bibliographic Details
Main Authors: Yuri L. Rebetsky, Anastasia V. Mikhailova
Format: Article
Language:English
Published: Institute of the Earth's crust, Siberian Branch of RAS 2015-09-01
Series:Geodinamika i Tektonofizika
Subjects:
gravity stress state
deviator stresses
cataclastic flow
initial stresses
evolution of the stress­and­strain state
horizontal shear
fractures
riedel shears
yield stress
Online Access:https://www.gt-crust.ru/jour/article/view/123

Internet

https://www.gt-crust.ru/jour/article/view/123

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