Fluid inclusions: evidence for a counterclockwise P-T trajectory in the Central Maine terrane of South-Central Massachusetts
Acadian (Late Silurian-Early Devonian) metamorphism in the Central Maine Terrane (CMT) in central Massachusetts is characterized by an early low-P, high-T (Buchan-type) metamorphism followed by compression and nearly isobaric cooling to 100-200°C below peak recorded temperatures before eventual unro...
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| Format: | Others |
| Language: | en |
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Virginia Tech
2014
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| Online Access: | http://hdl.handle.net/10919/41106 http://scholar.lib.vt.edu/theses/available/etd-02132009-172529/ |