Evidence for a Second Generation of Magnesite in Martian Meteorite Allan Hills 84001Single-stage formation mechanisms for carbonate and other secondary minerals in ALH84001 are rapidly being revised to include multiple stages of carbonate growth and later thermal and mechanical events including alteration. In an effort to confirm some of these more complex histories we have been studying carbonate-bearing regions within this meteorite. Magnesitic carbonates found in contact with unique 'slab' carbonates in two thin sections of ALH84001 show indications of being of a later generation. The results of our observations help clarify the origins of the carbonate and related minerals in ALH84001, and how these minerals can be used to understand the history of interactions between the martian crust and its volatile inventory.
Document ID
20030111409
Acquisition Source
Headquarters
Document Type
Conference Paper
Authors
Corrigan, C. M. (Case Western Reserve Univ. Cleveland, OH, United States)
Harvey, R. P. (Case Western Reserve Univ. Cleveland, OH, United States)