The accommodation of large strains in the upper lithosphere of the earth and other solids by self-similar fault systems: the geometrical origin of b-Value
- 1 September 1983
- journal article
- Published by Springer Nature in Pure and Applied Geophysics
- Vol. 121 (5-6) , 761-815
- https://doi.org/10.1007/bf02590182
Abstract
No abstract availableKeywords
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