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- W311156744 abstract "Frontal thrusts (Holston Mountain, Great Smoky, Miller Cover, Cartersville, Emerson, Talladega) along the southern Appalachian foreland-hinterland transition form an anastomosing complex that results from outward propagation of hinterland thrusts. These frontal thrusts serve as the composite roof of a major series of active roof duplexes that surface in windows and footwall ramps from Virginia to Alabama (Teas-Coleman Store, Virginia, Mountain City window, Tennessee, Tuckaleechee Cove, Tennessee, Bartow-Sugar Hill, Georgia, Sleeping Giants Range, Alabama). Floor thrusts developed independently and are observable only in particular areas. Imbricates in all transition zone duplexes are composed of Lower Cambrian clastic and carbonate rocks, except in the Tuckaleechee Cover duplex, which consist of upper Knox carbonates and Middle Ordovician shales. Aggregate basement plus cover (basement, Ocoee Series, Chilhowee Group, Shady Dolomite, Rome Formation) thicknesses involved in the frontal roof complex range from about 2.5 km (Georgia) to a maximum of 10 km (Tennessee) to intermediate values of 5 km (Alabama and Virginia). The combination of an eastward step to a lower master detachment, ideal ratio of strong to weak units ranging from 1:1 to 3:1, and the increased overburden thickness attributable to the stacking of thrust sheets nucleated the duplexes in the transition zones. Palinspasticmore » reconstruction indicates transition zone duplexes were nucleated in rift basins along the Precambrian Paleozoic North American Continental margin.« less" @default.
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- W311156744 date "1985-01-01" @default.
- W311156744 modified "2023-09-23" @default.
- W311156744 title "Southern Appalachians foreland-hinterland transition and the boundary conditions of duplex nucleation" @default.
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