Anatectic Pegmatites of the Oxford Country Pegmatite Field, Maine, USA
In contrast to suggestions of previous research, MMGM researchers believe that the Oxford Country Pegmatite Field pegmatites formed by direct anatexis of the metasedimentary and migmatitic country rocks.
Information
Authors
Karen Webber; William B. "Skip" Simmons; Alexander U. Falster; Sarah Hanson
Date
September 30, 2019
Source
The Canadian Mineralogist
Source (Long)
The Canadian Mineralogist 57(5):811-815