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M. Marot, T. Monfret, M. Pardo, G. Ranalli and G. Nolet A double seismic zone in the subducting Juan Fernandez Ridge of the Nazca Plate (32°S), central Chile Journal of Geophysical Research: Solid Earth 118

Version of Record online: 8 JUL 2013 | DOI: 10.1002/jgrb.50240

Key Points

  • Geometry, extent and state of stress of the central Chilean DSZ are reported
  • Its geometry and extent appear linked to the flat slab and low thermal state
  • Its state of stress is dominated by the strong plate convergence

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