Tamaki, Kensaku; Yamamoto, Kiyohiko (1992): Stress field of basaltic rocks of ODP Hole 127-794C. PANGAEA, https://doi.org/10.1594/PANGAEA.778095, Supplement to: Tamaki, K; Yamamoto, K (1992): Estimating in-situ stress field from basaltic rock core samples of Hole 794C, Yamato Basin, Japan Sea. In: Tamaki, K; Suychiro, K; Allan, J; McWilliams, M; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 127/128(2), 1047-1059, https://doi.org/10.2973/odp.proc.sr.127128-2.225.1992
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We carried out an experiment to estimate in-situ stresses at ODP Hole 794C (water depth: 2809 m) from the basaltic core samples by deformation rate analysis (DRA). Site 794 is located at the northern end of the Yamato Basin and 70 km west of the eastern Japan Sea intraplate or interplate convergent zone. Stress previously applied to a rock specimen is identified in the inelastic strain behavior of the specimen under uniaxial compression by the method used. Natural remanent magnetization of the sample was also measured to get a reference for the orientation of the horizontal stresses. The vertical, maximum, and minimum horizontal in-situ stresses estimated at a depth of 582 mbsf are 36.4, 43.1, and 31.2 MPa, respectively. The average of the largest and the least horizontal stresses is nearly equal in value to the vertical stress. This suggests that the site is in the stress field of the strike slip regime at the depth, while the stress field of the reverse fault regime has been estimated from the focal mechanism solutions of the earthquakes whose hypocenters are located near or on the convergent boundary. The directions of the largest and the least horizontal stress are estimated to be northeast-southwest and in northwest-southeast, respectively, in taking account of rotation tectonics of the Japan Sea since its formation. The directions of the largest and the least horizontal stresses are opposite to those determined from the earthquakes. These discrepancies of our results with those from earthquakes may be due mainly to the fact that the site is not in the convergent zone.
Latitude: 40.190000 * Longitude: 138.231000
Date/Time Start: 1989-07-03T20:30:00 * Date/Time End: 1989-07-11T11:00:00
127-794C * Latitude: 40.190000 * Longitude: 138.231000 * Date/Time Start: 1989-07-03T20:30:00 * Date/Time End: 1989-07-11T11:00:00 * Elevation: -2820.0 m * Penetration: 653.7 m * Recovery: 33.21 m * Location: Japan Sea * Campaign: Leg127 * Basis: Joides Resolution * Device: Drilling/drill rig (DRILL) * Comment: 14 cores; 93.9 m cored; 0 m drilled; 35.4 % recovery
Datasets listed in this Collection
- Tamaki, K; Yamamoto, K (1992): (Table 1) Physical properties of ODP Hole 127-794C samples. https://doi.org/10.1594/PANGAEA.778091
- Tamaki, K; Yamamoto, K (1992): (Table 2) Young's modulus of ODP Hole 127-794C samples. https://doi.org/10.1594/PANGAEA.778093
- Tamaki, K; Yamamoto, K (1992): (Table 3) Correction of previously applied stress for the pore-pressure effect, ODP Hole 127-794C samples. https://doi.org/10.1594/PANGAEA.778094