Thermal effects of ridge subduction

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Earth and Planetary Science Letters, 44 (1979) 239-246. 239 ... Lamont-Doherty Geological Observatory of Columbia University, Palisades, NY 10964 (U.S.A.).
Earth and Planetary Science Letters, 44 (1979) 239-246

239

© Elsevier Scientific Publishing Company, Amsterdam - Printed in The Netherlands

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THERMAL EFFECTS OF RIDGE SUBDUCTION S T E P H E N E. D e L O N G

Department o f Geological Sciences, State University o f New York at Albany, Albany, NY 12222 (U.S.A.) W.M. S C H W A R Z

Department o f Physics, Union College, Schenectady, NY 12308 (U.S.A.) and R O G E R N. A N D E R S O N

Lamont-Doherty Geological Observatory o f Columbia University, Palisades, NY 10964 (U.S.A.)

Received January 29, 1979 Revised version received April 2, 1979

The temperature structure of a subduction zone during subduction of an oceanic spreading ridge has been calculated by a finite-difference procedure. The plates preceding and following the ridge crest into the trench had convergence rates of 90 and 20 mm/yr, respectively, corresponding to a spreading half-rate for the ridge of 35 mm/yr and to the velocity balance for a simple three-plate model of ridge subduction. Abrupt temperature increases in the range 50-500°C occur at shallow locations (~

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