Normal fault growth in layered basaltic rocks: the role of strain rate in fault evolution
Conceptual models for the evolution of dilatant faults in volcanic rift settings involve a step-wise growth pattern, involving upward propagation of subsurface faults, surface monocline formation, which are breached by subvertical, open faults. Immature, discontinuous normal faults are considered re...
| Main Authors: | , , , |
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| Format: | Other/Unknown Material |
| Language: | unknown |
| Published: |
California Digital Library (CDL)
2017
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.31223/osf.io/zmt54 |