Linking of regional and local hydrothermal systems in the mid-crust by shearing and faulting

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Abstract

The concentration of mass during regional metamorphism and metallogenesis requires interactions between regional and local hydrothermal systems that are scale- and time-dependent. During regional low- to medium-temperature metamorphism in which fluid flow is driven by broad thermal or mechanical gradients, fluid flow rates are (on average)

Author-supplied keywords

  • Deformation
  • Fault
  • Fluid flow
  • Mineralization
  • Permeability
  • Shear zone

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Authors

  • Nicholas H.S. Oliver

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