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The Early to Middle Cambrian Stansbury Basin preserves a palaeogeographic zonation from shallow shelf carbonates to extensional rift facies. Sedimentation occurred from about 540 Ma to at least 510 Ma, with a distinctive phase of thick rift sedimentation in the Kanmantoo Trough from 526 Ma. This dataset, provided by the Australian Ocean Data Network, describes the basin's tectonic framework and its potential for various types of mineralisation.
File formats are PDF and HTML; the dataset may be a report or document rather than a structured data table.