Chatham Deep Drift
type: MRGeoObject
type: Drift
modified: 2023-05-20T10:02:38Z
is part of: Southwest Pacific Basin
is influenced by: Deep Western Boundary Current
had primary source:
  was attributed to:
    label: Carter, L. and I. N. McCave (2002). Eastern New Zealand Drifts, Miocene-Recent. Deep-Water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics. D. A. V. Stow, C. J. Pudsey, J. A. Howe, J.-C. Faugères and A. R. Viana. London, Geological Society. 22: 385-407.
has geometry: http://marineregions.org/mrgid/30276/geometries

Southwest Pacific Basin
type: MRGeoObject
type: Basin

Deep Western Boundary Current
type: MRGeoObject
type: Current