A MODEL OF THE SELF-STRESS STATE OF THE SEDIMENTARY ROCK AND ITS APPLICATION TO ESTIMATION OF RESIDUAL EFFECTS

Based on analysis of modern concepts describing changes in the stress-and-strain state of rocks, it is revealed that the elastic energy is not fully released and residual/own stresses occur in core samples taken out of the rock massif.The paper describes a model aimed at explanation of causes for re...

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Bibliographic Details
Main Author: A. I. Moroz
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2015-09-01
Series:Геодинамика и тектонофизика
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Online Access:https://www.gt-crust.ru/jour/article/view/74
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