BEDROCK MAPPING OF THE WINCHENDON (1:25,000) QUADRANGLE (MA-NH): EVIDENCE FOR DISCONTINOUS DEFORMATION ALONG THE BRONSON HILL-CENTRAL MAINE BOUNDARY ZONE
Bedrock geology of the Winchendon quadrangle is divided into two zones based on structures and lithology. The eastern zone consists of tightly folded Silurian Rangeley and Paxton metasediments and pegmatites. Planar, NNE-SSW striking, W dipping foliations are characterized by alternating phyllosilic...
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| Format: | Others |
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UKnowledge
2009
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| Online Access: | http://uknowledge.uky.edu/gradschool_theses/615 http://uknowledge.uky.edu/cgi/viewcontent.cgi?article=1619&context=gradschool_theses |