Velocity anomalies: An alternative explanation based on data from laboratory experiments
Pure and Applied Geophysics PAGEOPH
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Abstract
Locations and velocities were calculated for microseisms occurring in samples of rock subjected to triaxial loading and injection of pore fluid. This was accomplished by analyzing arrival times of acoustic emission using an automatic first arrival picker. Apparent velocity anomalies were observed prior to both failure of intact samples and violent slip in samples containing saw cuts. Further analysis revealed that these fluctuations in calculated velocity were not due to changes in the true seismie velocity. Instead, variations in calculated velocity are shown to be related to sampling errors in picking first arrivals. The systematic picking of late first arrivals for small magnitude events was found to be a persistent bias resulting in low calculated velocities. This has encouraged the reexamination of earthquake records to determine how important sampling biases are in contributing to reported velocity anomalies. ?? 1978 Birkha??user Verlag.
Suggested Citation
Lockner, D., Byerlee, J., 1978, Velocity anomalies: An alternative explanation based on data from laboratory experiments: Pure and Applied Geophysics PAGEOPH, v. 116, no. 4-5, p. 765-772, https://doi.org/10.1007/BF00876537.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Velocity anomalies: An alternative explanation based on data from laboratory experiments |
| Series title | Pure and Applied Geophysics PAGEOPH |
| DOI | 10.1007/BF00876537 |
| Volume | 116 |
| Issue | 4-5 |
| Year Published | 1978 |
| Language | English |
| Publisher location | Birkha??user-Verlag |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Pure and Applied Geophysics PAGEOPH |
| First page | 765 |
| Last page | 772 |