Key points are not available for this paper at this time.
The only two Nakhlite meteorites, Nakhla and Lafayette, are identical in mineral composition, consisting of augite (Wo 39 En 38 Fs 23 ), olivine (Fo 32–35 ), plagioclase (An 27 ), K‐feldspar (Or 75 Ab 22 An 3 ), titaniferous magnetite with exsolved ilmenite, iddingsite (?), and minor amounts of fluor‐chlorapatite, FeS, pyrite, chalcopyrite, and K‐rich glass. The texture is suggestive of a cumulative origin.
Bunch et al. (Mon,) studied this question.