Late Pleistocene-Holocene activity and paleoseismicity of the Nojima Fault in the northern Awaji Island, southwest Japan

Field investigations and analyses of tectonic landforms show that the topographical markers of terrace risers and alluvial fans formed in the late Pleistocene-Holocene have been systematically offset by ~40–62 m along the Nojima Fault on which the 1995 Mw 6.9 Kobe earthquake occurred. Analysis of te...

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Veröffentlicht in:Tectonophysics 2018-11, Vol.747-748, p.402-415
1. Verfasser: Lin, Aiming
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Sprache:eng
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