Canterbury D9
type: MRGeoObject
type: Drift
modified: 2013-07-22T06:17:17Z
is part of: Canterbury Drifts
is influenced by: Subantarctic Mode Water
had primary source:
  was attributed to: Lu, H., et al. (2003). Three-dimensional architecture of shelf-building sediment drifts in the offshore Canterbury Basin, New Zealand. Marine Geology 193: 19-47.

Canterbury Drifts
type: MRGeoObject
type: ContouriteDepositionalSystem

Subantarctic Mode Water
type: MRGeoObject
type: WaterMass