Loading...
Loading...
Available on 1 platform
Sign in to view source links and access this dataset
South Australia's Early to Middle Cambrian Stansbury Basin preserves a paleogeographic zonation from shallow shelf carbonates to extensional rift facies. Sedimentation occurred from about 540 Ma to at least 510 Ma, with a phase of thick rift sedimentation from 526 Ma. The dataset from Geoscience Australia describes the basin's tectonic evolution and potential for various mineral deposit types, including Mississippi Valley-type and volcanogenic massive sulphide mineralisation.
License is unknown; terms of use should be verified before application.