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to continent-facing normal faults.
*10 to 15 km thick bodies in the lower crust (HVLC) show high seismic P-Wave velocities, between 7.1 and 7.8 km/s which lie under the transitional crust (crust between continental crust and oceanic crust).
*Seaward Dipping Reflector (SDR) series: Inner SDRs overlie transitional continental crust.

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