Fluid-induced seismicity: comparison of rate- and state- and critical pressure theory
Abstract Induced seismicity as generated by the injection of fluids in a homogeneous, permeable medium with faults with variable proximity to rupture conditions is simulated using the rate- and state-dependent frictional fault theory (RST) of Dieterich (J Geophys Res 99(B2):2601–2618, 1994) and the...
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| Format: | Article |
| Language: | English |
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SpringerOpen
2017-06-01
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| Series: | Geothermal Energy |
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| Online Access: | http://link.springer.com/article/10.1186/s40517-017-0063-2 |