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Absolute far-field displacements from the 28 June 1992 Landers earthquake sequenceDisplacements observed for the Landers earthquake indicate that the depth of the bottom of the rupture is shallower towards the northern end. Displacements were dominantly symmetric and the rupture extended farther south on the Johnson Valley fault than has been mapped on the basis of surface ground offsets. The combined geodetic moment for the Landers and Big Bear earthquakes agrees well with teleseismic estimates.
Document ID
19930042246
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Blewitt, Geoffrey
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Heflin, Michael B.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Hurst, Kenneth J.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Jefferson, David C.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Webb, Frank H.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Zumberge, James F.
(JPL Pasadena, CA, United States)
Date Acquired
August 16, 2013
Publication Date
January 28, 1993
Publication Information
Publication: Nature
Volume: 361
Issue: 6410
ISSN: 0028-0836
Subject Category
Geophysics
Accession Number
93A26243
Distribution Limits
Public
Copyright
Other

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