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Evidence of Non-Linear Elasticity of the Crust from the Mw7.6 Manyi (Tibet) Earthquake Surface Displacement FieldSatellite synthetic aperture radar (SAR) interferometry shows that the magnitude 7.6 Manyi earthquake of 8 November 1997 produces a 170 km-long surface break with up to 7m of left-lateral slip, reactivating a North 76 degrees East quaternary fault in western Tibet.
Document ID
20060034192
Acquisition Source
Jet Propulsion Laboratory
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Peltzer, G.
Crampe, F.
King, G.
Date Acquired
August 23, 2013
Publication Date
August 1, 1999
Publication Information
Publication: Science
Distribution Limits
Public
Copyright
Other
Keywords
SAR Interferometry Earthquake

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