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The out‐of‐sequence thrust and the frontal thrust can be identified as a discontinuity in the displacement of the particles in the model.To illuminate clearly the stress change, the slip tendency (ST) (defined as the shear stress divided by normal stress) is calculated in the model. The slip tendency around the OOST is higher before a large slip event than those after the event, suggesting that the...
The degree of gas hydrate saturation at Integrated Ocean Drilling Program (IODP) Site C0002 in the Kumano Basin, Nankai Trough, was estimated from logging‐while‐drilling logs and core samples obtained during IODP Expeditions 314 and 315. Sediment porosity data necessary for the calculation of saturation were obtained from both core samples and density logs. Two forms of the Archie equation (‘quick‐look’...
Tectonic inversion is a common phenomenon in island arc settings, especially in back‐arc basins. The reactivation of normal faults as thrusts, triggered by tectonic inversion, produces typical inversion fault‐related folds and thrusts in the hangingwall. These hangingwall inversion geometries are affected by two factors: the geometry of the underlying master fault and the angle of inclined simple...
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