Geochronology and Petrology of Coronitic Metagabbro and Garnetiferous Amphibolite in the Adirondack Mountains, Newcomb, New York
The Adirondack Mountains form the southern extension of the Grenville Province, an orogeny that formed during the formation of supercontinent Rodinia in the late Mesoproterozoic. This orogenesis can be defined by three major phases over 250 million years: the Elzevirian (1245 – 1225 Ma), the Shawini...
| Main Authors: | , |
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| Format: | Other/Unknown Material |
| Language: | unknown |
| Published: |
2021
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| Subjects: | |
| Online Access: | https://hdl.handle.net/20.500.13013/1519 |