The Occurrence of Garnet in the Granulite-Facies Terrane of the Adirondack Highlands
- 1 January 1965
- journal article
- Published by Oxford University Press (OUP) in Journal of Petrology
- Vol. 6 (1) , 165-191
- https://doi.org/10.1093/petrology/6.1.165
Abstract
Based on the presence or absence of almandine in charnockitic and metabasic rocks, Buddington (1963) recognized two garnet isograds in the northwestern Adirondacks which were inferred to represent a general increase in grade of regional metamorphism from northwest to southeast and east.Keywords
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