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Unconformity related and deep burial diagenesis, Upper Knox carbonates, southern and central Appalachians

Conference · · Geol. Soc. Am., Abstr. Programs; (United States)
OSTI ID:6458759

Early cemented Upper Knox (pre-unconformity) carbonates appear to have escaped much subsequent diagenesis, possibly due to early loss of permeability. A regional unconfined aquifer system accompanied the Knox unconformity,from which it was sourced. Waters moving rapidly by free flow through developing cavern systems, were undersaturated with respect to both aragonite and calcite resulting in large scale dissolution of limestone interbeds and development of interstratal-karstic collapse breccias. Localized concentrations of intrastratal karst below the unconformity may relate to a paleowater table or a paleo-mixing zone. Aquifer stagnation and precipitation of Fe and Mn-rich cements probably accompanied Middle Ordovician transgression and subsequent sedimentation. Middle Ordovician uplift along the eastern basin margin generated tectonic highlands that sourced meteoric fluids which moved downdip in a confined aquifer, flushing earlier stagnant porewater depositing a second generation of nonluminescent cement. Increasing burial beneath thick foreland basin clastics resulted in aquifer stagnation and dull cement precipitation. Episodic dewatering of Appalachian basinal shales was accompanied by rapid migration of warm, saline brines. Fluids moving along earlier intrastratal karstic conduits resulted in localized dissolution of carbonates and massive brecciation of intrastratal karst fills. Major porosity reduction occurred by precipitation of Fe-poor saddle dolomite, locally interstratified with sphalerite and associated minor hydrocarbons. Latest cements are minor Fe-rich calcite and silica.

Research Organization:
Virginia Tech, Blacksburg (USA)
OSTI ID:
6458759
Report Number(s):
CONF-8510489-
Journal Information:
Geol. Soc. Am., Abstr. Programs; (United States), Journal Name: Geol. Soc. Am., Abstr. Programs; (United States) Vol. 17; ISSN GAAPB
Country of Publication:
United States
Language:
English