Tracing causes for the stress sensitivity of elastic wave velocities in dry Castlegate sandstone
The stress sensitivity of elastic wave velocities in dry rock is a resultant of two types of processes-elastic and non-elastic processes. Both processes are activated under stress and both are associated with stress-induced changes in the rock structure. Although they are of the same origin, their s...
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| Veröffentlicht in: | Geophysical journal international 2013, Vol.192 (1), p.137-147 |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
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