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Near-isothermal conditions in the middle and lower crust induced by melt migration

Author

Listed:
  • Gabriela V. Depine

    (Snee Hall, Cornell University, Ithaca, New York 14853, USA)

  • Christopher L. Andronicos

    (Snee Hall, Cornell University, Ithaca, New York 14853, USA)

  • Jason Phipps-Morgan

    (Snee Hall, Cornell University, Ithaca, New York 14853, USA)

Abstract

Simple one-dimensional thermal models that include the effects of melt migration have been developed. The models show that long-lived plutonism results in a quasi-steady-state geotherm with a rapid temperature increase in the upper crust and nearly isothermal conditions in the middle and lower crust.

Suggested Citation

  • Gabriela V. Depine & Christopher L. Andronicos & Jason Phipps-Morgan, 2008. "Near-isothermal conditions in the middle and lower crust induced by melt migration," Nature, Nature, vol. 452(7183), pages 80-83, March.
  • Handle: RePEc:nat:nature:v:452:y:2008:i:7183:d:10.1038_nature06689
    DOI: 10.1038/nature06689
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