Magmatic subsidence of the East Pacific Rise ( EPR ) at 18 14 0 S revealed through fault restoration of ridge crest bathymetry

@inproceedings{Carbotte2003MagmaticSO,
  title={Magmatic subsidence of the East Pacific Rise ( EPR ) at 18 14 0 S revealed through fault restoration of ridge crest bathymetry},
  author={Suzanne Carbotte and William B. F. Ryan and Wen Jun Jin and Marie-Helene Cormier and E. C. Bergmanis and John M. Sinton},
  year={2003}
}
[1] The fault restoration technique of De Chabalier and Avouac [1994] is applied to an ultra-highresolution bathymetry data set from the East Pacific Rise (EPR) at 18 140S. Fault offsets are calculated and subtracted from the original seafloor bathymetry to examine the morphology of the unfaulted seafloor surface within an area encompassing the ridge axis 40 

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