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Updated: Aug 9, 2026

Simulation of the Planetary Interior Differentiation Processes in the Laboratory
Published on: November 15, 2013
Simulation of subduction zone seismicity by dehydration of serpentine
David P Dobson1, Philip G Meredith, Stephen A Boon
1Bayerisches Geoinstitut, Universität Bayreuth, D-95440 Bayreuth, Germany. d.dobson@ucl.ac.uk
Abstract:
We measured acoustic emission energy during antigorite dehydration in a multianvil press from 1.5 to 8.5 gigapascals and 300 degrees to 900 degrees C. There was a strong acoustic emission signal on dehydration, and analysis of recovered samples revealed brittle deformation features associated with high pore-fluid pressures. These results demonstrate that intermediate depth (50 to 200 kilometers) seismicity can be generated by dehydration reactions in the subducting slab.
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