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The fracture of a rock mass is an important stage in the development of catastrophes in a block system. In this paper, the characteristics of P-wave propagation in block rock mass containing fault block are investigated experimentally. Velocity of P-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa382034be95e38fa0842020abf95642
https://doi.org/10.21203/rs.3.rs-2692132/v1
https://doi.org/10.21203/rs.3.rs-2692132/v1
