Northwest Africa 2526: A partial melt residue of enstatite chondrite parentage |
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| Authors: | Klaus KEIL Addi BISCHOFF |
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| Institution: | 1. Hawai'i Institute of Geophysics and Planetology, School of Ocean and Earth Science and Technology, University of Hawai'i at Manoa, Honolulu, Hawai'i 96822, USA;2. Institut für Planetologie, Westf?lische Wilhelms‐Universit?t, Wilhelm‐Klemm‐Str. 10, 48149 Münster, Germany |
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| Abstract: | 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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