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Title: Igneous history of the aubrite parent asteroid - evidence from the Norton County enstatite achondrite

Journal Article · · Meteoritics; (United States)

Numerous specimens of the Norton County enstatite achondrite (aubrite) were studied by optical microscopy, electron microprobe, and neutron-activation analysis. Norton County is found to be a fragmental impact breccia, consisting of a clastic matrix made mostly of crushed enstatite, into which are embedded a variety of mineral and lithic clasts of both igneous and impact melt origin. The Norton County precursor materials were igneous rocks, mostly plutonic orthopyroxenites, not grains formed by condensation from the solar nebula. The Mg-silicate-rich aubrite parent body experienced extensive melting and igneous differentiation, causing formation of diverse lithologies including dunites, plutonic orthopyroxenites, plutonic pyroxenites, and plagioclase-silica rocks. The presence of impact melt breccias (the microporphyritic clasts and the diopside-plagioclase-silica clast) of still different compositions further attests to the lithologic diversity of the aubrite parent body. 60 references.

Research Organization:
Institute of Physical and Chemical Research, Wako (Japan); New Mexico Univ., Albuquerque (USA)
OSTI ID:
6921001
Journal Information:
Meteoritics; (United States), Vol. 23
Country of Publication:
United States
Language:
English