A prediction of mars seismicity from surface faulting
The shallow seismicity of Mars has been estimated by measurement of the total slip on faults visible on the surface of the planet throughout geologic time. Seismicity was calibrated with estimates based on surface structures on the moon and measured lunar seismicity that includes the entire seismogenic lithosphere. Results indicate that Mars is seismically active today, with a sufficient number of detectable marsquakes to allow seismic investigations of its interior.
Citation Information
Publication Year | 1992 |
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Title | A prediction of mars seismicity from surface faulting |
Authors | M.P. Golombek, W.B. Banerdt, K. L. Tanaka, D.M. Tralli |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Science |
Index ID | 70017246 |
Record Source | USGS Publications Warehouse |