Abstract
Geoelectric surveys are made in areas of probable seismic segment boundaries along the Yangsan fault zone (between 36.2°N and 35.5°N) in order to investigate resistivity structure. These segment boundaries are proposed on the basis of reduced seismicity recorded in historical earthquake data. Wenner horizontal profilings reveal resistivity of about 300 ohm-m with electrode separation of 30 m, which compares with that of 100 ohm-m in other parts of the Yangsan fault zone. Schlumberger vertical soundings indicate that the fault fracture zone diminishes in depth from about 100 m (north) to 20 m (south). Previous vertical soundings in other parts of the Yangsan fault zone show that the fault fracture zone extends to a depth greater than 100 m. Electrical profilings and soundings appear to indicate poor development of fault fractures in the study area. Geoelectrical surveys support the existence of boundaries between the northern and the central segments as well as between the central and the southern seismic segments in the Yangsan fault zone.
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Lee, K., Lee, J. Geoelectric study on the probable seismic segment boundaries of Yangsan fault zone. Geosci J 1, 16–25 (1997). https://doi.org/10.1007/BF02910446
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DOI: https://doi.org/10.1007/BF02910446