Abstract
We have detected a 30,000-square-kilometer area rich in olivine in the Nili Fossae region of Mars. Nili Fossae has been interpreted as a complex of grabens and fractures related to the formation of the Isidis impact basin. We propose that post-impact faulting of this area has exposed subsurface layers rich in olivine. Linear mixture analysis of Thermal Emission Spectrometer spectra shows surface exposures of 30% olivine, where the composition of the olivine ranges from Fo30 to Fo70.
Original language | English (US) |
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Pages (from-to) | 627-630 |
Number of pages | 4 |
Journal | Science |
Volume | 302 |
Issue number | 5645 |
DOIs | |
State | Published - Oct 24 2003 |
ASJC Scopus subject areas
- General