Sentence examples for slip segment from inspiring English sources

Our inversion analysis suggests that the strain accumulation rate for the right-lateral seismic slip segment (corresponding to the Futagawa fault), where the largest of the 2016 Kumamoto earthquakes ruptured, was several times smaller than the other segments in the Beppu−Shimabara graben.

The large slip segments are in located in four separate areas.

They found that the morphology of the so-called flower structure (Harding 1990) on N-S seismic profiles is indicative of a transition of active strike-slip segments on the MTL.

Hence, the source density is ndcs=ρs/rdcs, where the pinning length of the cross slipped segments is of the order of the dislocation spacing, (r_{text {dcs}} = 1/sqrt {{rho ^{text {tot}}}}) with ({rho ^{text {tot}}} = sum _{varsigma } rho ).

Dextral-reverse slip on segment a of the Beichuan fault becomes partitioned into a dextral dominant component on segment b of the Beichuan fault and thrust-dominant component on segment e of the Guanxian fault (Fig. 4).

In addition, the large seismic moment released by the previous large earthquakes and the subsequent slow slip in Segment B acted as a barrier to prevent the extension of both the 2011 Tohoku mainshock rupture and its aftershock activity (Kosuga and Watanabe, 2011).

"Slip lemon segments into your water or herbal tea to refresh your drink and help you digest fat… Then to boost your five a day, eat the lemon afterwards".

Results of near-field tsunami records strongly support anomalously large slips in Segment C′ (e.g., Maeda et al., 2011).

Under these circumstances, the GNSS monitoring network in southwest Japan has revealed a variety of slow slip events segmented along the Suruga and Nankai trough subduction zones.

Owing to the associated crustal vertical deformation, the down-dip extension of large slip on segments beneath Shikoku Island induces tsunamis higher than a few meters in the Seto Inland Sea region.

This indicates that slip on segments B and C, with a maximum of about 10 m (see green contours in Figure 3b), cannot explain the historical damage records for the Pacific coast in the Kinki region.