Petrology of 78155 - An early, thermally metamorphosed polymict breccia
Polymict breccia 78155, which has a bulk composition of anorthositic norite, was brecciated and thermally metamorphosed before the final lunar bombardment of 4.0-3.9 eons. The constituents of the granoblastic matrix and the characteristics of the clasts and the mafic silicates are described. The clasts represent the lunar crust prior to 4.2 eons, the age of the granoblastic matrix. The persistence of uninverted pigeonite in matrix and clasts indicates that metamorphism was at a very high temperature and may have been terminated catastrophically. Evidence that the rock was further brecciated after thermal metamorphism is reported.