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• W2016684558 startingPage "333" @default.
• W2016684558 abstract "Abstract— Ureilites are modeled as impact-melt products of CV-chondrite-like material. This model is consistent with the brecciated nature and cumulate textures of ureilites, O-isotopic constraints (which indicate ureilite derivation from an isotopically heterogeneous body like the CV-chondrite parent), the high abundance of planetary-type noble gases, and the relatively high concentrations of siderophile and chalcophile elements (indicating incomplete separation of metal-sulfide from silicate). Each ureilite may have been derived from a separate cratering event." @default.
• W2016684558 created "2016-06-24" @default.
• W2016684558 creator A5034637836 @default.
• W2016684558 date "1988-12-01" @default.
• W2016684558 modified "2023-09-24" @default.
• W2016684558 title "Formation of Ureilites by Impact-Melting of Carbonaceous Chondritic Material" @default.
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• W2016684558 doi "https://doi.org/10.1111/j.1945-5100.1988.tb00918.x" @default.
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