Evolution of tectono-sedimentary systems in the Kumano Basin , Nankai Trough forearc

@inproceedings{Moore2015EvolutionOT,
  title={Evolution of tectono-sedimentary systems in the Kumano Basin , Nankai Trough forearc},
  author={Gregory F. Moore and Barry Boston and Michael Strasser and Michael B. Underwood and Roosevelt Ratliff},
  year={2015}
}
Sedimentary deposits in the distal Kumano forearc basin of the Nankai accretionary margin off Kii Peninsula, Japan, have been imaged using three-dimensional (3D) seismic data. The seismic data, along with logging and core data from the Integrated Ocean Drilling Program (IODP) show that the unconformity between the accretionary prism and overlying forearc sediments is time-transgressive. The unconformity at Site C0002 separates 5 Ma prism rocks from 3.65 Ma basin deposits; at Site C0009 it… CONTINUE READING

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