Wind-reworked fluvial deposits as an archaeological environment: the Agnes Banks Sand of the Quaternary Hawkesbury–Nepean sequence of southeast Australia
Author:
Affiliation:
1. Department of Archaeology, The University of Sydney, Sydney, Australia
2. School of Geosciences, The University of Sydney, Sydney, Australia
Publisher
Informa UK Limited
Subject
Earth-Surface Processes,Geography, Planning and Development
Link
https://www.tandfonline.com/doi/pdf/10.1080/00049182.2023.2250157
Reference90 articles.
1. Ahlbrandt, T. S. 1979. “Textural Parameters of Eolian Deposits.” In A Study of Global Sand Seas, edited by E. D. McKee, 21–51. Washington DC: United States Geological Survey Professional Paper 1052.
2. Provenance, diagenesis, tectonic setting and geochemistry of Hawkesbury Sandstone (Middle Triassic), southern Sydney Basin, Australia
3. Floodplain sedimentation: Quantities, patterns and processes
4. A multivariate analysis of alluvial terrace soils of the clarendon and cranebrook formations, Nepean River, NSW
5. Baker C. J. 1977. “Geological Assessment of the Pitt Town High Level Sand Deposit.” Geological Survey of New South Wales Report GS 1977/139: 1–7.
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