The thermal structure of subduction zone back arcs

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Reply to comment by W. P. Schellart on ‘‘The thermal structure of subduction zone back arcs’’

[1] Currie and Hyndman [2006] documented the evidence that the majority of continental back arcs are uniformly hot with thin lithospheres over regional extents of hundreds of kilometers, even if where is no thermally significant extension. Using a number of independent observations, we showed that eight such current subduction zones have similar thermal regimes, with Moho temperatures greater t...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research

سال: 2006

ISSN: 0148-0227

DOI: 10.1029/2005jb004024