1887

Abstract

Summary

It is proposed to determine the direction of the “main stress” based on the study of the deformation and acoustic properties of full-size core samples with its subsequent binding to the side of the world using the paleomagnetic method. The methodology of the experiments, the equipment used for this purpose, and the results obtained are described.

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/content/papers/10.3997/2214-4609.201900526
2019-03-25
2024-04-26
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