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• W1965278548 endingPage "190" @default.
• W1965278548 startingPage "181" @default.
• W1965278548 abstract "Magnetic spinels produced by oxidation of extraterrestrial objects in the atmosphere have a composition distinct from terrestrial spinels. They are characterized by a high iron oxidation state, arising from crystallization under high oxygen fugacities, and a high nickel concentration due to the relatively high abundance of this element in extraterrestrial material. The iron oxidation state increases from micrometeorites, to meteoroid ablation material and to impact-generated products. This reflects a progressive increase of the oxygen fugacity, corresponding to decreasing altitudes of crystallization. Spinels found at the Cretaceous-Tertiary boundary are similar to those that crystallized from meteoroid ablation material and impact-generated products, supporting the view that a collisional event did occur at the end of the Cretaceous." @default.
• W1965278548 created "2016-06-24" @default.
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• W1965278548 date "1992-02-01" @default.
• W1965278548 modified "2023-10-17" @default.
• W1965278548 title "Formation of spinels in cosmic objects during atmospheric entry: a clue to the Cretaceous-Tertiary boundary event" @default.
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• W1965278548 doi "https://doi.org/10.1016/0012-821x(92)90021-m" @default.
• W1965278548 hasPublicationYear "1992" @default.
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