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- W8142890 abstract "The Pine Mountain window is the most southern and internal Grenville basement massif in the Appalachian Mountain chain that retains its primary miogeoclinal stratigraphic cover. Previously metamorphosed billion-year-old granite gneisses have a modified stratigraphic contact with a younger metasedimentary sequence interpreted to correspond with either the upper Precambrian Ocoee Supergroup or Cambrian Weisner-Shady sequence of the Blue Ridge. Middle to upper amphibolite-facies assemblages in cover rocks sharply contrast with granulite-facies assemblages reported for basement units, which were retrograded to amphibolite-facies assemblages possibly as a result of thrust emplacement of the Inner Piedmont terrane during the middle to late Paleozoic. Late Paleozoic right-slip faulting, characterized by midcrustal-level mylonites with subvertical foliations and shallow NE-plunging elongation lineations, was pervasive throughout the basement/cover complex in Alabama and apparently overprinted earlier thrust zones. Right-slip faulting, possibly aided by ramping along lower, as yet unroofed thrusts, elevated the basement/cover contact to its present-day high structural level. It is unknown at present how far displaced the Pine Mountain window is from its original paleogeographic position along the ancient Laurentian margin." @default.
- W8142890 created "2016-06-24" @default.
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- W8142890 date "1992-01-01" @default.
- W8142890 modified "2023-09-26" @default.
- W8142890 title "The Pine Mountain window of Alabama: Basement-cover evolution in the southernmost exposed Appalachians" @default.
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- W8142890 doi "https://doi.org/10.1007/978-94-011-1614-5_33" @default.
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