Secondary Minerals in the Nakhlite Meteorite Yamato 000593: Distinguishing Martian from Terrestrial Alteration Products

The nakhlites are olivine-bearing clinopyroxenites that formed in a Martian lava flow or shallow intrusion 1.3 Ga ago [1, 2]. They are scientifically extremely valuable because they interacted with water-bearing fluids on Mars [3]. Fluid-rock interactions led to the precipitation of secondary minera...

Full description

Bibliographic Details
Main Authors: Breton, H., Lee, M.R., Mark, D.F.
Format: Conference Object
Language:English
Published: 2015
Subjects:
Online Access:http://eprints.gla.ac.uk/102426/
http://eprints.gla.ac.uk/102426/1/102426.pdf