Laboratory observation of slow movements in rocks

Laboratory observation of slow movements in rocks

Bibliographic Details
Parent link:Journal of Applied Mechanics and Technical Physics: Scientific Journal
Vol. 52, iss. 3.— 2012.— [P. 467-470]
Other Authors: Zuev L. B., Barannikova S. A., Zhigalkin V. M., Nadezhkin M. V. Mikhail Vladimirovich
Summary:Title screen
It is established that the development of a localized plastic strain during compression of samples of rocks (sylvinite, marble, and sandstone) deformed by different micromechanisms has an autowave character. It is shown that the velocity of propagation of autowaves arising in the samples under compression is 10?5 to 10?4 m/s (0.3 to 3.0 km/g) and is close to the velocity of slow waves observed in the Earth’s crust after earthquakes or rockbursts
Режим доступа: по договору с организацией-держателем ресурса
Language:English
Published: 2012
Subjects:
электронный ресурс
труды учёных ТПУ
rocks
autowaves
Online Access:http://link.springer.com/article/10.1134/S0021894412030200
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=637127

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