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Itoh et al. (1998) interpreted the spatiotemporal changes in the fault activity as transitions of active segments of the MTL.
Spatiotemporal changes in fault activity (transitions of the active MTL segments), migration of the depocenters in Beppu Bay, and emergence of the newly found inversion phase are to be linked to the tectonic regimes on the convergent margin.
The stress fluctuations due to such fault behavior can only be observed around active faults, and no fluctuation can be identified once fault activity has ceased.
Contacts with the enclosing host rocks showed fault activity, he pointed out.
The paleotectonic stress tensor is determined using fault activity analysis, acoustic emission tests, and burial history.
A decline in fault activity would have taken place after 30.8 ka.
Some previous studies propose that the present cliff morphology was mainly originated by Quaternary fault activity.
A type of fault activity called block faulting, in which the movement is predominantly vertical, began to form the valley about 30 million years ago.
Several shoals observed along the transgressive surface could record minor deformation due to fault activity in the study area.
It is suggested to estimate the Pliocene–Quaternary fault activity in a formalized way from synthesis of different data.
Although N S fault activity has already been established, we propose its significant contribution to shaping the landscape.
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