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- W2116853722 abstract "The timing and geometry of late Palaeozoic inhomogenous deformation in the southern U.S. continental interior from the Appalachian foreland of Kentucky-Tennessee through Oklahoma and Texas to the Ancestral Rockies of Colorado-Wyoming-Utah can be definitively linked with a discrete sequence of collisional events in the Appalachian-Ouachita-Marathon orogenic belt to the south (Permian coordinates). A progressive staged collisional sequence beginning in late Mississippian times in the southern Appalachians and culminating in early Permian times in the Marathons led to a progressive deformation of the adjacent craton in a wide swath dominated by right-lateral shear (e.g. Rough Creek Fault zone) by which a Mexican promontory of North America was displaced towards a Pacific ‘free face’. While the deformation in the Appalachian-Marathon belt was dominated by vertical plane strain leading to crustal thickening, the associated continental interior deformation can be averaged as a horizontal plane strain at or near sea level with localized deep extensions (Delaware) and flexural (Arkoma) basins and compressions uplifts (Amarillo-Wichita) giving local source areas." @default.
- W2116853722 created "2016-06-24" @default.
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- W2116853722 date "1982-05-05" @default.
- W2116853722 modified "2023-09-25" @default.
- W2116853722 title "Late Palaeozoic basins of the southern U.S. continental interior" @default.
- W2116853722 doi "https://doi.org/10.1098/rsta.1982.0030" @default.
- W2116853722 hasPublicationYear "1982" @default.
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