Shallow subsurface deformation along the Pen Branch Fault in South Carolina: interpretation from seismic refraction stack sections
The Pen Branch Fault is a reactivated, high angle, reverse basin border fault that dips to southeast from the basement (Triassic-Paleozoic-Precambrian in age) to near vertical through the Atlantic Coastal Plain sediments (Late Cretaceous to Recent in age) of the Savannah River site in South Carolina...
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| Format: | Others |
| Language: | en |
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Virginia Tech
2014
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| Online Access: | http://hdl.handle.net/10919/44797 http://scholar.lib.vt.edu/theses/available/etd-09182008-063212/ |