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Sean D. Willett and Mark T. Brandon Some analytical methods for converting thermochronometric age to erosion rate Geochemistry, Geophysics, Geosystems 14

Version of Record online: 31 JAN 2013 | DOI: 10.1029/2012GC004279

Key Points

  • Addresses problem of conversion of a cooling age to an exhumation rate
  • Combines solutions of exhuming half-space with closure temperature
  • Introduces graphical method for solving problem and estimating uncertainty

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