Wiso Basin
Lithology: | Sedimentary: dolostone, limestone, shale, sandstone, siltstone. | |
Epoch Min: | Devonian. | |
Epoch Max: | Cambrian. | |
Age Min: | 360 Ma. | |
Age Max: | 540 Ma. | |
Summary: | An intracratonic basin initiated as part of the Centralian Superbasin. The basin deepens toward the south (Lander Trough) along the margin with the Aileron Province. | |
Relationship: | Faulted against Palaeo-Neoproterozoic metamorphic rocks of the Aileron Province to the south. Unconformably overlies Palaeoproterozoic rocks of the Tanami Region to the west, Tennant Region to the east, and the Palaeo-Mesoproterozoic Birrindudu Basin to the northwest. Cretaceous rocks of the Carpentaria Basin cover its northern margin. | |
Thickness: | Up to 3 km in the Lander Trough, generally less than 300m elsewhere. | |
Economic: | Rare oil shows in stratigraphic holes. Gas shows in waterbores. | |
Metamorphism: | Unmetamorphosed. | |
Main Reference: | Kruse PD and Munson TJ, 2013. Chapter 32: Wiso Basin: in Ahmad M and Munson TJ (compilers) ‘Geology and Mineral Resources of the Northern Territory’. Northern Territory Geological Survey, Special Publication 5 |
Give feedback about this page.
Share this page:
URL copied!