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Paleoaquifer and deep burial related cements defined by regional cathodoluminescent patterns, Middle Ordovician Carbonates, Virginia/sup 1/

Journal Article · · AAPG Bull.; (United States)
OSTI ID:5236228
Middle Ordovician ramp carbonates, Virginia, were deposited in a subsiding, foreland basin bordered on the southeast by tectonic highlands. Ramp carbonates were lithified, in part, by turbid marine cements, but major cementation was by nonferroan, clear rim, and equant cements. Zoned (defined by cathodoluminescence) clear cements consist of nonluminescent (oldest), bright, and dull (youngest) cements; the zonation relates to increasingly reducing conditions of pore waters. Zoned cements in peritidal beds, best developed in southeastern belts, have complex zonations, pendant to pore-rimming fabrics, and are associated with crystal silt (which abuts all cement zones), solutional cavities, and erosional surfaces (which locally truncate dull cement). These cements are meteoric vadose to shallow phreatic. Cements in northwestern exposures of peritidal beds are dominated by nonzoned, dull cement which lacks abundant evidence of early, near-surface precipitation. Major cementation of subtidal facies occurred under burial conditions. Burial cements, best developed in southeastern belts, have a simple zonation reflecting progressive burial (up to 7.5 km; 4.5 mi) of the carbonate ramp. Shallow burial nonluminescent cement formed from oxidizing, meteoric waters which expelled anoxic, connate marine waters.
Research Organization:
Virginia Polytechnic and State Univ., Blacksburg, VA
OSTI ID:
5236228
Journal Information:
AAPG Bull.; (United States), Journal Name: AAPG Bull.; (United States) Vol. 67:8; ISSN AABUD
Country of Publication:
United States
Language:
English