Non-tectonic faults due to landslide movement and their mechanism

It might be relatively easy to discern non-tectonic faults from tectonic ones, if they die out toward the depth, or their dipping angle is low like a sliding surface of landslide and the texture and/or rock facies of the hanging wall is completely different from those of the foot wall. Faults observ...

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Bibliographische Detailangaben

Veröffentlicht in:	Journal of the Japan Landslide Society 2007, Vol.44 (4), p.205-213
Hauptverfasser:	NOZAKI, Tamotsu, OOJI, Akihito, HOSONO, Mayumi
Format:	Artikel
Sprache:	eng
Schlagworte:	Faults Landslides Movement Rock Sliding Surface layer Tectonics Texture Walls
Online-Zugang:	Volltext
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