Lithologic Structure of the Anninghe Fault Zone: Constraints From High-Pressure Wave Velocity Experiments
The P-wave velocities of typical rocks in the Anninghe fault zone under pressures of 50–600 MPa were systematically measured. The P-wave velocities of the felsic, intermediate, and mafic rock types under atmospheric pressure were 5.86, 6.06, and 6.50 km/s, respectively, with pressure coefficients of...
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| Format: | Artigo |
| Sprache: | Inglês |
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Frontiers Media S.A.
2022-03-01
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| Schriftenreihe: | Frontiers in Earth Science |
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| Online-Zugang: | https://www.frontiersin.org/articles/10.3389/feart.2022.853474/full |
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