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- W1634985239 abstract "Recently, the eastern margin of the Japan Sea is remarked as a newly developed convergent boundary between Eurasian and North American plates (Nakamura, 1983). The assumed boundary is located from Fossa Magna along the Toyama Trough, Sado Ridge, Okushiri Ridge towards the western egde of Okhotsk Sea (Fig.1). Some features of subducting slab, that is, thrust faulting, are observed by seismic profiling survey in several places along the line, (Nakamura, 1983; Asada et al., 1989). The southernmost part of the Toyama Trough, however, shows no evidence of thrust faulting from the result of seismic profiling, although this is located just north of Fossa Magna, and so some active tectonic movement is expected. In fact, this place is characterized as low seismicity area on the whole, but recently plenty of earthquakes of M3 ~ 5 occur frequently, and the largest one (M5.9) was occured on March 24, 1987. The distribution of the hypocentres suggests the existence of thrust faulting across the Toyama Trough off Noto Peninsula according to the seismic data catalogue of Japan Meteorological Agency. Therefore, this area of the expected plate boundary was selected as a target of precise survey, and gravity measurement was conducted on the sea bottom across the trough by use of the Japanese deep sea research vessel “SHINKAI 2000” in 1987 and 1988. The authors would like to report the result of the sea bottom gravimetry at the Toyama Trough and discuss the sub-bottom structure derived from the gravity anomaly and its tectonic implications." @default.
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- W1634985239 date "1990-01-01" @default.
- W1634985239 modified "2023-09-27" @default.
- W1634985239 title "Gravity Measurement on the Bottom of Toyama Trough" @default.
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- W1634985239 doi "https://doi.org/10.1007/978-1-4612-3404-3_17" @default.
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