Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8136047 | Icarus | 2015 | 25 Pages |
Abstract
The detailed mineralogical analysis of the Marcia quadrangle indicates that this quadrangle is the result of the mixture of the Vestan “endogenic” minerals with the “exogenic” carbonaceous chondrites. The stratigraphic units around Marcia clearly show the bright, uncontaminated material interlaced and mixed with the dark material that contains a strong OH signature. Only few small areas can be considered as representative of the old Vestan original material.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Space and Planetary Science
Authors
M.C. De Sanctis, J.-P. Combe, A. Ammannito, A. Frigeri, A. Longobardo, E. Palomba, F. Tosi, F. Zambon, K. Stephan, C.A. Raymond, C.T. Russell,