Frederic L. Schwab; Origin of the Antietam Formation (late Precambrian?; lower Cambrian), central Virginia. Journal of Sedimentary Research ; 40 (1): 354–366. doi: https://doi.org/10.1306/74D71F46-2B21-11D7-8648000102C1865D
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Quartz-rich clastics, derived from low-lying complex of crystalline rocks and sediments to the west in the craton, paleocurrent analysis, current reworking insignificant, no southeast borderland source
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