Laboratory observation of slow movements in rocks View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2012-05

AUTHORS

L. B. Zuev, S. A. Barannikova, V. M. Zhigalkin, M. V. Nadezhkin

ABSTRACT

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. More... »

PAGES

467-470

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s0021894412030200

DOI

http://dx.doi.org/10.1134/s0021894412030200

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1053141476


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