Origins of clay-rich strata in Cenozoic paleochannel deposits: an example from Suttor Formation, Queensland
Author:
Affiliation:
1. School of Earth and Environmental Sciences, University of Queensland, Queensland, QLD, Australia
2. BHP, Brisbane, QLD, Australia
Funder
BHP BM Alliance Coal Operations Pty Ltd
Publisher
Informa UK Limited
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Link
https://www.tandfonline.com/doi/pdf/10.1080/08120099.2023.2127122
Reference48 articles.
1. Age of the Yarrabee and accessory tuffs: implications for the upper Permian sediment-accumulation rates across the Bowen Basin
2. Post-orogenic structural style and reactivation in the northern Bowen Basin, eastern Australia
3. The evolution of a Late Cretaceous–Cenozoic intraplate basin (Duaringa Basin), eastern Australia: evidence for the negative inversion of a pre-existing fold–thrust belt
4. Beeston, J. W. (1994). Tertiary palynology in the Mount Coolon and Riverside areas. Queensland Geology, 6, 127–179.
5. Clay Sedimentology
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