Aioun EL Atrouss - Evidence for thermal recrystallization of a eucrite breccia

Details Aioun EL Atrouss - Evidence for thermal recrystallization of a eucrite breccia Aioun EL Atrouss - Evidence for thermal recrystallization of a eucrite breccia

Dec 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978metic..13..443d&link_type=abstract

(Meteoritical Society, Annual Meeting, 41st, Sudbury, Ontario, Canada, Aug. 14-17, 1978.) Meteoritics, vol. 13, Dec. 31, 1978, p

Physics

2

Breccia, Meteoritic Composition, Mineralogy, Recrystallization, Basalt, Chronology, Meteoritic Microstructures, Textures

Scientific paper

The Aioun el Atrouss meteorite is a breccia consisting largely of angular fragments of green orthopyroxene and containing scattered clasts of basaltic composition (mostly pigeonite and calcic plagioclase). It appears to be a physical mixture of two meteorite types - diogenite (hypersthene achondrite) and eucrite (basaltic achondrite). The results of a mineral analysis are tabulated, and typical pyroxene compositions in orthopyroxene (diogenite), subophitic and granoblastic portions of the meteorite are presented.

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