Abstract

Discussion of a paper by C.W. Fortson and A.T. Navarre (Geoscience Abstracts 1-3142). Monazite bearing rocks are abundant, not rare. The pegmatite masses at one locality are not in shear zones but are in a plunging anticline. The host rock at a second locality is coronite, not amphibolite. It is not possible to confirm the existence of rhyolite, phyllite, or breccia.

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