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martian wrinkle ridge topography: evidence for subsurface faults from molaMars Orbiter Laser Altimeter (MOLA) profiles across wrinkle ridges are characterized by plains surfaces at different elevations on either side that appear best explained by subsurface thrust faults that underlie the ridges and produce the offset.
Document ID
20000080995
Document Type
Conference Paper
Authors
Golombek, M. P.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Anderson, F. S.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Zuber, M. T.
(Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA United States)
Date Acquired
August 19, 2013
Publication Date
March 1, 2000
Publication Information
Publication: Lunar and Planetary Science XXXI
Subject Category
Lunar and Planetary Science and Exploration
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.

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