1. The sequence architecture of mid-Pleistocene (c. 1.1–0.4 Ma) cyclothems from New Zealand: facies development during a period of orbital control on sea-level cyclicity;Abbott;Special Publication of the International Association of Sedimentologists,1994
2. The influence of aggradation on braided alluvial architecture: field study and physical scale-modelling of the Ashburton River gravels, Canterbury Plains, New Zealand;Ashworth;Special Publication of the International Association of Sedimentologists,1999
3. Bal, A.A., 1997. The stratigraphic and sedimentologic characteristics of gravel lithofacies, coastal Canterbury, New Zealand, as encountered in a water bore, Seafield. Unpublished Client Report 51653A.10b. Institute of Geological and Nuclear Sciences, 19 pp.
4. High-frequency sequences deposited during Quaternary sea-level cycles on a deforming continental shelf, north Canterbury, New Zealand;Barnes;Sedimentary Geology,1995
5. Quaternary alluvial plain construction in response to glacio-eustatic and climatic controls, Texas Gulf coastal plain;Blum;SEPM Special Publication,1998