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Holly M. M. Rotman and Glenn A. Spinelli Global analysis of the effect of fluid flow on subduction zone temperatures Geochemistry, Geophysics, Geosystems 14

Version of Record online: 30 AUG 2013 | DOI: 10.1002/ggge.20205

Key Points

  • Fluid circulation significantly cools subduction zones with young lithosphere
  • Cooling is maximized for slow convergence and steeply dipping slabs
  • Hydrothermal cooling is important if subduction zone thermal parameter <500 km

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