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Paleozoic carbonate gravity-flow deposits, and relationships to changes of relative sea level, Southernmost Appalachians

Conference ·
OSTI ID:6592029
The Jumbo Dolomite, deposited during a sea level fall at the end of the Early Ordovician, consists of lenticular carbonate masses embedded in the Mount Zion Formation, basinal shales deposited seaward of a Cambrian-Early Ordovician carbonate shelf. Stacked gravity-flow deposits include: (1) early massive debris-flow beds, with allogenic carbonate, chert, and sandstone clasts in a micritic matrix; (2) thick to massive debris-flow beds, with authigenic clasts in an argillaceous micritic matrix; and (3) late, fine-grained carbonate turbidites with partial Bouma sequences. Interbedded basinal shales (Bouma E) are more numerous in the upper part of this third unit. Gravity-flow deposits in the Athens (Middle Ordovician) and Floyd (mid-Mississippian) Shales were deposited during sea level rises. Argillaceous micrite turbidities in the Athens were derived from shallower bathymetric levels of a carbonate ramp. Gravity-flow deposits in the Floyd are individual tabular debris flows of skeletal debris and authigenic shale clasts in a micritic argillaceous matrix. Discrete gravity-flow beds deposited during sea level rises may be attributed to platform margin collapses. Stacking of flow deposits in the Jumbo indicates point-sourced flows localized by channels. The succession in the Jumbo represents stages in the fall, stabilization, and rise of sea level relative to the shelf; unit 1 represents early exposure and erosion of the shelf, and units 2 and 3 indicate the cessation of coarse debris input as a low-relief subaerial surface developed and sea level stabilized. Interbedded shales near the top of unit 3 represent sediment starvation associated with the subsequent rise of relative sea level.
OSTI ID:
6592029
Report Number(s):
CONF-880301-
Country of Publication:
United States
Language:
English

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