Evolution of the intracratonic Officer Basin, central Australia: implications from subsidence analysis and gravity modelling
The intracratonic basins of central Australia are distinguished by their large negative Bouguer gravity anomalies, despite the absence of any significant topography. Over the Neoproterozoic to Palaeozoic Officer Basin, the anomalies attain a peak negative amplitude in excess of 150 mGal, amongst the...
| Main Authors: | , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
2001
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