Tectonic evolution of the southern Appalachian Inner Piedmont: Identification and interpretation of crustal features from aeromagnetic data and detailed geologic mapping in central Georgia
The Inner Piedmont (IP) is the Neoacadian migmatitic orogenic core of the southern Appalachians, exhibiting the widest area of high-grade metamorphism; regional upper amphibolite facies with isolated pods of granulite grade metamorphism. Peak P-T conditions in central GA reached 4.0-7.6 kbars and 63...
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Format: | Others |
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Trace: Tennessee Research and Creative Exchange
2010
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Online Access: | http://trace.tennessee.edu/utk_gradthes/617 |