High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spine...
High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
About this item
Full title
Author / Creator
Publisher
Washington: Mineralogical Society of America
Journal title
Language
English
Formats
Publication information
Publisher
Washington: Mineralogical Society of America
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More information
Scope and Contents
Contents
We quantify the metamorphic pressure-temperature (P-T) conditions for a newly discovered silica-undersaturated high-pressure granulite (HPG) from the Central Maine Terrane (CMT) in northeastern Connecticut, U.S.A. The rocks lie within the Acadian-Neoacadian orogenic belt (Devonian) and form part of the Brimfield Schist. The Brimfield and the adjace...
Alternative Titles
Full title
High-pressure granulite facies metamorphism (1.8 GPa) revealed in silica-undersaturated garnet-spinel-corundum gneiss, Central Maine Terrane, Connecticut, U.S.A
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_proquest_journals_2282038307
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2282038307
Other Identifiers
ISSN
0003-004X
E-ISSN
1945-3027
DOI
10.2138/am-2018-6543
