Anisotropy of Partial Anhysteretic Remanent                 Magnetization: Application to Rock Deformation Studies
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The PIs will investigate an hypothesis that the anisotropic                acquisition of certain remanent magnetizations will be                          insensitive to mineralogical variation, and will thus be solely                 controlled by the degree of particle alignment.  Remanent                       anisotropies therefore ought to provide a much clearer indication               of principal strain magnitudes.  Partial anhysteretic remanent                  magnetization (pARM), which has been shown to be an effective                   means of recognizing grain-size variation in magnetite, can be                  potentially used to estimate the degree of particle alignment as                a function of grain size.
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[{'Code': '1572', 'Text': 'Tectonics'}, {'Code': '1574', 'Text': 'Geophysics'}]
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