NASA Logo

NTRS

NTRS - NASA Technical Reports Server

Back to Results
Detection of aseismic creep along the San Andreas fault near Parkfield, California with ERS-1 radar interferometryThe differential interferometric analysis of ERS data from Parkfield (CA) observations revealed the wide area distribution of creep along the moving fault segment of the San Andreas fault over a 15 month interval. The removal of the interferometric phase related to the surface topography was carried out. The fault was clearly visible in the differential interferogram. The magnitude of the tropospheric water vapor phase distortions is greater than the signal and hinders quantitative analysis beyond order of magnitude calculations.
Document ID
19980216261
Document Type
Conference Paper
Authors
Werner, Charles L. (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Rosen, Paul (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Hensley, Scott (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Fielding, Eric (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Buckley, Sean (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Date Acquired
August 18, 2013
Publication Date
May 1, 1997
Publication Information
Publication: Proceedings of the 3rd ERS Symposium on Space at the Service of Our Environment, volume 1
Volume: 1
Subject Category
Geophysics
Distribution Limits
Public
Copyright
Other
Document Inquiry