Sedimentology of the Unicoi Formation in southern and central Virginia: evidence for late Proterozoic to Early Cambrian rift-to- passive margin transition

  • Simpson E
  • Eriksson K
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Abstract

Records the transition from late Proterozoic to Early Cambrian rifting to initial opening of the Iapetus Ocean. The rift-to-passive margin phases of sedimentation in the central Appalachians reflect a continuum from fault-influenced to thermotectonic subsidence. -from Authors

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