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The late Cainozoic evolution of the Carpentaria Plains, North Queensland: a discussion

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Created 20/01/2025

Updated 20/01/2025

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Grimes and Doutch (1978) have identified five predominantly alluvial stages in the depositional landforms of the Carpentaria Plains. In the light of the factors which they consider to be the most likely controls on the evolution of the plains, they suggest a correlation between these stages, sea-level, climatic changes, and other depositional sequences in Queensland.

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Title The late Cainozoic evolution of the Carpentaria Plains, North Queensland: a discussion
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/66f5e3ba-bf38-4e2b-87b9-3b9fa28a24ba
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[138.0, -29.2], [154.0, -29.2], [154.0, -10.0], [138.0, -10.0], [138.0, -29.2]]]}
Data Portal data.gov.au

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This dataset was originally found on data.gov.au "The late Cainozoic evolution of the Carpentaria Plains, North Queensland: a discussion". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/the-late-cainozoic-evolution-of-the-carpentaria-plains-north-queensland-a-discussion