A Crustal Rock Clast in Magnesian Anorthositic Breccia, Dhofar 489 and Its Excavation from a Large Basin

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Scientific paper

From the older Ar-Ar age (4.27 Gyr) and the presence of a spinel
troctolite clast in Dhofar 489, we propose that a large basin formation
other than Imbrium may have mixed deep crustal rocks and "pure"
anorthosites to produce a magnesian breccia.

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