Garnetites of the Cardigan Pluton - Evidence for Restite and Implications for Source Rock Compositions.
The Cardigan pluton, located in the southern half of New Hampshire, is a strongly peraluminous, S-type granite which is granodioritic in composition. It is inferred to have been emplaced rapidly, thrust up along west-verging nappes during the Acadian orogeny. Distinctive pods, consisting of 50 to 70...
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| Format: | Others |
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BYU ScholarsArchive
2006
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| Online Access: | https://scholarsarchive.byu.edu/etd/1099 https://scholarsarchive.byu.edu/cgi/viewcontent.cgi?article=2098&context=etd |
