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WAVES IN THE VISCOUS FLOW OF THE FRICTIONAL CLAY IN THE FAULT AS A MECHANISM OF THE RUPTURE-LIKE REGIME OF POSTGLACIAL REBOUND
Journal: Geophysical research
Tome: 12
Number: 3
Year: 2011
Pages: 49-54
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Gavrilov S. WAVES IN THE VISCOUS FLOW OF THE FRICTIONAL CLAY IN THE FAULT AS A MECHANISM OF THE RUPTURE-LIKE REGIME OF POSTGLACIAL REBOUND // . 2011. Т. 12. № 3. С. 49-54.
@article{GavrilovWAVES2011,
author = "Gavrilov, S.",
title = "WAVES IN THE VISCOUS FLOW OF THE FRICTIONAL CLAY IN THE FAULT AS A MECHANISM OF THE RUPTURE-LIKE REGIME OF POSTGLACIAL REBOUND",
journal = "Geophysical research",
year = 2011,
volume = "12",
number = "3",
pages = "49-54",
doi = "",
language = "English"
}
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Keywords: postglacial rebound, rupture-like slip on fault, instability of convective flow
Аnnotation: WAVES IN THE VISCOUS FLOW OF THE FRICTIONAL CLAY IN THE FAULT AS A MECHANISM OF THE RUPTURE-LIKE REGIME OF POSTGLACIAL REBOUND
