The Hadley Rille enstatite chondrite and its agglutinate-like rim: Impact melting during accretion to the Moon

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Impact-induced melting during accretion of the Earth

Because of the high energies involved, giant impacts that occur during planetary accretion cause large degrees of melting. The depth of melting in the target body after each collision determines the pressure and temperature conditions of metal-silicate equilibration and thus geochemical fractionation that results from core-mantle differentiation. The accretional collisions involved in forming t...

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ژورنال

عنوان ژورنال: Meteoritics & Planetary Science

سال: 1997

ISSN: 1086-9379,1945-5100

DOI: 10.1111/j.1945-5100.1997.tb01248.x