2002Lunar and Planetary Science ConferenceRequires access

Petrographic Studies of Sulfide Assemblages in the Allende CV3 Carbonaceous Chondrite

Chris Wetteland, A. J. Brearley

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Abstract

Studies of sulfides in Allende show that pyrrhotite occurs mainly within chondrules and has been partially replaced by pentlandite. Ni and Co contents of pentlandites within individual chondrules are homogeneous, but are variable between chondrules. Additional information is contained in the original extended abstract.

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What this paper is about

Studies of sulfides in Allende show that pyrrhotite occurs mainly within chondrules and has been partially replaced by pentlandite. Ni and Co contents of pentlandites within individual chondrules are homogeneous, but are variable between chondrules. Additional information is contained in the original extended abstract.

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Available abstract

Studies of sulfides in Allende show that pyrrhotite occurs mainly within chondrules and has been partially replaced by pentlandite. Ni and Co contents of pentlandites within individual chondrules are homogeneous, but are variable between chondrules. Additional information is contained in the original extended abstract.

Key concepts: Allende meteorite, Chondrule, Chondrite, Pentlandite, Petrography, Carbonaceous chondrite, Geology, Geochemistry

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