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Morphostructural evolution of active margin basins: the example of the Hawke Bay forearc basin, New Zealand.
(University of Canterbury. Geological Sciences, 2007)
Topography growth and sediment fluxes in active subduction margin settings are poorly understood. Geological record is often scarce or hardly accessible as a result of intensive deformation. The Hawke Bay forearc basin of ...
Mid-Pleistocene Extinction of Deep-Sea Ostracoda?
(University of Canterbury. Geological Sciences, 2006)
A global extinction event has been documented in protozoan foraminifera in the late Pliocene to Pleistocene. The timing of the extinction event varied depending on location, however for Ocean Drilling Project Site 1125, ...