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April 01, 1999
The classic high-T--low-P metamorphism of west-central Maine; is it post-tectonic or syntectonic? Evidence from porphyroblast-matrix relations Available to Purchase
G. S. Solar;
G. S. Solar
University of Maryland, Laboratory for Crustal Petrology, College Park, MD, United States
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G. S. Solar
University of Maryland, Laboratory for Crustal Petrology, College Park, MD, United States
M. Brown
Publisher: Mineralogical Association of Canada
First Online:
02 Mar 2017
Online ISSN: 1499-1276
Print ISSN: 0008-4476
© 1999 Mineralogical Association of Canada
The Canadian Mineralogist (1999) 37 (2): 311–333.
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First Online:
02 Mar 2017
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CitationG. S. Solar, M. Brown; The classic high-T--low-P metamorphism of west-central Maine; is it post-tectonic or syntectonic? Evidence from porphyroblast-matrix relations. The Canadian Mineralogist 1999;; 37 (2): 311–333. doi:
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Index Terms/Descriptors
- Devonian
- fabric
- granites
- granulometry
- high temperature
- igneous rocks
- intrusions
- low pressure
- Maine
- matrix
- metamorphism
- mineral composition
- Paleozoic
- paragenesis
- petrography
- plutonic rocks
- plutons
- porphyroblastic texture
- pressure
- regional metamorphism
- structural analysis
- syntectonic processes
- tectonic elements
- tectonics
- temperature
- textures
- United States
- Central Maine Belt
Latitude & Longitude
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