QuaternaryScienceReviews

New Paper in Qua­ter­nary Science Reviews

Charlotte Pizer´s latest research integrating onshore-offshore paleoseismic record reveal multiple slip styles on the plate interface, central Hikurangi subduction margin.

Results reveal widespread, synchronous triggering of turbidity currents only occurs when coastal coseismic deformation is recorded. Onshore-offshore earthquake evidence shows past earthquakes vary in their size, location and combination of source faults.

Read the full paper here

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