Geochemistry of the Sykesville diamictite in central Maryland: an investigation of clast-matrix activity during metamorphism with tectonic implications
The Sykesville diamictite is part of the Wissahickon sequence, a polydeformed and metamorphosed sequence of questionable age in the Central Appalachian Piedmont. It occurs in association with thrust stacks of volcanic and mafic units of the Baltimore Mafic Complex and Potomac Valley Sequence in Mary...
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| Format: | Others |
| Language: | en_US |
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Virginia Polytechnic Institute and State University
2019
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| Online Access: | http://hdl.handle.net/10919/94480 |