Fault stability inferred from granite sliding experiments at hydrothermal conditions
Geophysical Research Letters
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Abstract
Seismicity on crustal faults is concentrated in the depth interval 1–3 to 12–15km. Tse and Rice (1986) suggested that the lower bound on seismicity is due to a switch with increasing temperature from velocity weakening (destabilizing) to velocity strengthening (stabilizing) friction. They inferred this transition from friction data for dry granite; however, pore fluids exist at elevated temperatures throughout the crust, and may strongly influence strength and sliding behavior. We present new data from sliding experiments on granite at elevated T (23° to 600°) plus elevated PH2O (100 MPa),
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Fault stability inferred from granite sliding experiments at hydrothermal conditions |
| Series title | Geophysical Research Letters |
| DOI | 10.1029/91GL00469 |
| Volume | 18 |
| Issue | 4 |
| Year Published | 1991 |
| Language | English |
| Publisher | American Geophysical Union |
| Description | 4 p. |
| Larger Work Type | Article |
| First page | 609 |
| Last page | 612 |
| Google Analytic Metrics | Metrics page |