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Many normal faults cut across the folds in various directions.
It is characterized by many normal faults formed in the N S extensional stress regime.
The MCS record for ECr31 shows many normal faults beneath the Miyako Saddle and the Kerama Gap.
In Miocene when Japan-sea was opened, many normal faults are formed under the extensional stress regime.
Two distinctive reflectors at depths of 1 2 and 3 4 km were observed beneath the Miyako Saddle, and they are cut by many normal faults.
Many normal faults and transform faults formed during the several stages of evolution of the Shikoku Basin have been observed in previous bathymetric, geomagnetic and seismic reflection surveys (e.g., Chamot-Rooke et al. 1987; Okino et al. 1994).
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Branches, relays, and conjugate faults are found in many normal fault populations (Peacock 2002; Morley et al. 2007; Nicol et al. 1995; Walsh et al. 1999).
Previous studies (e.g., Asano et al. 2011) analyzed seismicity immediately after the 2011 Tohoku-oki earthquake and reported the occurrence of many normal fault aftershocks.
It is found that earthquakes were mainly reverse fault type events all over the source region before the main shock, whereas, after the main shock, many normal fault type events occurred in the hanging wall but focal mechanisms did not change in the deepest part in the source region.
The effect of the western rift margin of the Indian plate dominance can be observed in the form of many normal fault and horst and associated grabens on the seismic sections and also in the form of Sibbi-Jacobabbad, Khairpur, Mari-Kandkot highs as its surface expressions (Michalchuk 2006).
The border of the Fukushima and Ibaraki prefectures, where many normal-fault aftershocks are observed, has a ΔCFF of 0.5– 1.0 MPa.
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