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The document discusses a study of the crustal structure around the fault zone of the 1938 M 6.0 Kutcharo earthquake in northern Japan using gravity anomalies, magnetotelluric and electrical resistivity data. The results indicate that the earthquake fault was located along the main depression boundary of the Kutcharo caldera, corresponding to boundaries between resistivity blocks. A detailed resistivity section also showed a discontinuity of layers along the fault zone, implying cumulative displacements occu
- Author
- agusitampan
- Language
- EN