slow slip
Recovery of the recurrence interval of Boso slow slip events in Japan
... main slip area of the Boso slip, although some of the main slip area showed a slightly negative ΔCFS (Additional file 1: Figure ...main slow slip area by Hirose et ...
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Configuration and structure of the Philippine Sea Plate off Boso, Japan: constraints on the shallow subduction kinematics, seismicity, and slow slip events
... with slow slip events off Boso, ...Boso slow slip ...Boso slow slip events, which indicates that the slow slip area and regular low- angle thrust earthquakes are ...
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Long term slow slip event detected beneath the Shima Peninsula, central Japan, from GNSS data
... of slow earth- quakes. Long-term slow slip events (SSEs), with dura- tions of months or years, have been observed by using data from the global navigation satellite system (GNSS) in the Bungo Channel ...
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Detection of small crustal deformation caused by slow slip events in southwest Japan using GNSS and tremor data
... fault slip rates between the fast rupture of a regular earthquake and stable sliding, have also been detected by dense geodetic and seismological observa- ...tion. Slow slip events (SSEs), which ...
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Laterally propagating slow slip events in a rate and state friction model with a velocity-weakening to velocity-strengthening transition
... with a velocity-weakening to velocity-strengthening transi- tion is relevant for the part of the plate interface between the locked and steadily sliding regions. Such a friction law is consistent with one common physical ...
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Occurrence of quasi periodic slow slip off the east coast of the Boso peninsula, Central Japan
... estimated slow-slips, the slow-slips are the primary process driving eathquake swarms, as was the case of the previous Boso slow-slip events and the case of the Salton Trough, California, ...
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A slow slip event in the Tokai area detected by tilt and seismic observation and its possible recurrence
... A major question still remains as to whether tilt or other deformation observations can detect precursors. A discour- aging example is the Tokachi-Oki earthquake (M8.0) on September 26, 2003, which did not provide us ...
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Statistic analysis of swarm activities around the Boso Peninsula, Japan: Slow slip events beneath Tokyo Bay?
... by slow slip events (SSEs) and found that stressing rate controls the background seismicity μ suggesting that swarms can be utilized to monitor stress change due to various aseismic ...
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A long term slow slip event from 1996 to 1997 in the Kii Channel, Japan
... Various types of slow slip events (SSEs) have been reported along subduction plate boundaries. These events tend to exhibit large variations in duration, mag- nitude, and recurrence behavior (Schwartz and ...
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Long term slow slip events along the Nankai trough subduction zone after the 2011 Tohoku earthquake in Japan
... Bungo slow slip was occurring between May 1, 2014, and October 1, 2014 ...Miyazaki slow slips (Fig. 4b). This slow slip was very small compared with the 1997, 2003, and 2010 Bungo ...
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Repeating short and long term slow slip events with deep tremor activity around the Bungo channel region, southwest Japan
... long-term slow slip events (SSE) which are accompanied by deep tremor activity around the Bungo channel region, southwest ...‘slow slip patches’ on a plate interface, where the episodic ...
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Preceding seismic activity and slow slip events in the source area of the 2011 Mw 9.0 Tohoku-Oki earthquake: a review
... accelerated slow slip) in the downdip portion of the source area on the megathrust ...postseismic slip (dotted curves) is apparent in the figure ...
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Two long term slow slip events around Tokyo Bay found by GNSS observation during 1996–2011
... Slow slip events (SSEs) with durations ranging from days to more than a decade have been observed in plate sub- duction zones around the ...fault slip corresponded well with increases in the ...
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Objective detection of long term slow slip events along the Nankai Trough using GNSS data (1996–2016)
... long-term slow slip events with durations on the order of years, on the plate boundary along the Nankai Trough, relying on global navigation satellite system daily coordinate ...long-term slow ...
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Possible slow slip event beneath the Kii Peninsula, southwest Japan, inferred from historical tilt records in 1973
... recurrent slow slip events (SSEs) in many subduction ...a slow transient signal down to the northeast of about ...a slip amount larger than that in the template models, which suggests that the ...
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Slow slip in the focal region of the anticipated Tokai earthquake following the seismo volcanic event in the northern Izu Islands in 2000
... forward slip exceeds the secular convergence rate from June to September and July to October but did not occur from May to August, suggest that the ongoing Tokai slow event found by Ozawa et ...Tokai ...
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Elastic interaction of parallel rate and state dependent frictional faults with aging and slip laws: slow slip faults can sometimes host fast events
... In contrast to surface observation of complex earthquake faults, simple fault-plane models are frequently sufficient to fit geophysical data of seismic wave or crustal deformation. However, earthquake occurrence should ...
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A possible restart of an interplate slow slip adjacent to the Tokai seismic gap in Japan
... Fig. 2d–f may be directly comparable to the second data- set. All the GPS sites in Fig. 2d–f show southeastward or eastward displacements from early 2013. Figure 3 shows the characteristic features of the spatial ...
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Spatial and temporal evolution of the long term slow slip in the Bungo Channel, Japan
... aseismic slip area shifted to beneath the southwestern part of Shikoku, adjacent to the area ruptured by the 1946 Nankai earthquake ...the slow slip in the west and central parts of the Bungo Channel ...
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Interval modulation of recurrent slow slip events by two types of earthquake loading
... Geodetic studies have discovered recurrent spontaneous slow slip events (SSEs) at major faults. The SSE recurrence intervals should reflect stress states at the faults, including load effects of large ...
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