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.

First Page Preview

First page PDF preview
You do not currently have access to this article.