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- W1497392323 abstract "The geometries and facies distributions of siliciclastic and carbonate sand bodies in Lower Silurian strata of the southern Appalachian Basin of east Tennessee reflect the complex interaction of storm processes within shoreface and shallow-marine shelf environments. The shallower and more proximal siliciclastic shoreface consisted of megaripples and sand waves that migrated northwestward under the influence of offshore-directed storm currents. Within the inner and middle shelf environments, combined storm-wave oscillatory flows and along-shelf geostrophic(?) flows deposited storm sand sheets containing varying scales of hummocky cross-stratification and wave-ripple lamination, which are interbedded with variable proportions of non-bioturbated mudstone. The outer shelf was dominated by non-bioturbated mudstone. A carbonate storm-shelf system existed contemporaneously to the west of the bathymetric basin axis. Storm-generated currents transported coarse skeletal sand eastward into the terrigenous-mud-dominated basin centre resulting in deposition of carbonate storm sand sheets into a ‘background’ mudstone lithology. Thus, basin-wide facies geometry consists of a central terrigenous-mudstone-dominated facies, into which a regressive, upward-shoaling sandstone wedge and associated facies prograded from the southeast, and carbonate sand sheets contemporaneously extended into the basin from the northwest." @default.
- W1497392323 created "2016-06-24" @default.
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- W1497392323 date "1992-01-30" @default.
- W1497392323 modified "2023-09-27" @default.
- W1497392323 title "Model for Genesis of Shoreface and Shelf Sandstone Sequences, Southern Appalachians: Palaeoenvironmental Reconstruction of an Early Silurian Shelf System" @default.
- W1497392323 doi "https://doi.org/10.1002/9781444303933.ch9" @default.
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