The Piermont allochthon revisited and redefined at its type locality
Regional lithostratigraphic and structural mapping of the Piermont allochthon of northwestern New England at its type locality indicates that the Foster Hill fault, the supposed sole thrust, is a stratigraphic boundary. Rather, the allochthon lies above the Bean Brook fault, covers a much smaller ar...
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| Format: | Journal Article |
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Geological Society of America
2004
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| Online Access: | http://hdl.handle.net/20.500.11937/29755 |
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