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Deep-sea drilling expedition off Japan to probe microbial boundary beneath sea floor.
On the interplate boundary beneath MRT2, the seismic refraction study detected a subducting seamount (Kodaira et al. 2000) (light blue ellipse in Figure 7).
However, the depth of the Philippine Sea slab is almost similar to that of the Moho boundary beneath the faults of Nobi earthquake (Nakajima et al. 2015).
Ishihara et al. (1981) suggested that the anomaly reflects either an uplift of the Moho boundary beneath the Bonin ridge, or the presence of a high-density crust beneath the ridge.
In this research, we estimate the spatiotemporal evolution of the aseismic slip along the plate boundary beneath the Bungo Channel area since January 2009 and compare it with previous long-term slow slips.
Within the study period, there were no unsteady displacements related to the sources of long-term slow slip on the plate boundary beneath the Kii Peninsula and central Shikoku.
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The shape of many grains becomes irregular, and the grain boundaries beneath the machined surface slide in response to the exerted cutting forces.
Because previous studies mainly used data from land-based stations alone, the shallow parts of the PAC NA and PHS NA boundaries beneath the area offshore of the Boso Peninsula (particularly trenchward from 141°E) have not yet been defined.
Along the Magnus-Rex Line 3, the structure of the crust is characterised by almost horizontal layering with a local uplift of the major crustal boundaries beneath the Oslo Graben (Stratford et al. [2009], Stratford and Thybo [2011]).
Fig. 9 Time variations in the modeled pressure increments at selected sites on the plate boundary, located beneath R1, R2, and R4.
In this easternmost plate boundary region beneath TOK1, no major earthquake has occurred in the past 160 years since the last historical earthquake in 1854 (Ando 1975).
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