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Institute of Seismology and Volcanology
Hokkaido University
Sapporo 060-0810, Japan
(K.K., M.Ka., M.I.)
Earthquake Research Institute
University of Tokyo
Tokyo 113-0032, Japan
(M.Ki.)
Institute of Marine Geology and Geophysics
Russian Academy of Science
Yuzhno-Sakhalinsk, Russia
(C.-U.K., A.I.)
Institute of Physics of the Earth
Russian Academy of Science
123810 Moscow, B. Gruzinskaya 10, Russia
(R.T.)
On 27 May 1995, a large earthquake (Ms 7.6) occurred in the northern part of Sakhalin Island near an uncertain plate boundary between the Okhotsk (or the North American) plate and the Eurasian (or the Amurian) plate. The source process of the mainshock, the detailed aftershock activity, the b-value of the frequencymagnitude relationship for aftershocks, and the 3D P-wave velocity distribution have been investigated. Thirty-one body-wave records were inverted to determine the sequence of subevents of the mainshock using an iterative deconvolution method. The source parameters obtained are the location of the initial epicenter (52.64° N, 142.83° E); the centroid depth (9 km); strike, dip, and slip, equal to (191°, 87°, 172°) for the first subevent, (198°, 76°, 175°) for a second subevent, and (196°, 79°, 174°) for the combined source; and the total seismic moment M0 (4.2 x 1019 N m) and Mw (7.0). We also deployed 12 temporary seismographic stations in the focal area from 7 June to 8 July 1995. More than 2000 events were located in an aftershock area of 60 km x 10 km that trends in a N15°E direction, which is consistent with the location of the surface rupture tracing the Gyrgylan'iOssoy fault. The P-wave velocity patterns were compared with the aftershock seismicity and the spatial distribution of the b-values, with results suggesting that high velocity correlates with high seismicity and small b-value. Our research strongly suggests that the 1995 Sakhalin earthquake was one of the outstanding events that define the uncertain plate boundary.
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