Gravity and Magnetics

We combine gravity and magnetics with remote sensing lineaments, seismic, and structure, to

  1. determine the orientation and extent of basment faults obsevred on seismic
  2. suggest faults in regions where no outcrop or lineament data exist
  3. differentiate which lineaments are related to major basment faults.
Using these integrated data sets, we have been able to propose numerous fault systems across the Appalachian Plateau of NYS. Click here to see Figure 8a
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