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Northwest Africa 2526: A partial melt residue of enstatite chondrite parentage

Meteoritics and Planetary Science (2008) 43(7) 1233-1240
DOI: 10.1111/j.1945-5100.2008.tb01125.x
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Abstract

NWA 2526 is a coarse-grained, achondritic rock dominated by equigranular grains of polysynthetically twinned enstatite (∼85 vol%) with frequent 120° triple junctions and ∼10-15 vol% of kamacite + terrestrial weathering products. All other phases including troilite, daubreelite, schreibersite, and silica-normative melt areas make up

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Keil, K., & Bischoff, A. (2008). Northwest Africa 2526: A partial melt residue of enstatite chondrite parentage. Meteoritics and Planetary Science, 43(7), 1233–1240. https://doi.org/10.1111/j.1945-5100.2008.tb01125.x

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