Cambrian Stansbury Basin Tectonic and Metallogenic Framework, South Australia

540 to at least 510 million years ago, sedimentation occurred in the Cambrian Stansbury Basin of South Australia. The dataset, likely compiled by geological researchers, describes the basin's tectonic evolution and potential for mineral deposits like Mississippi Valley-type and volcanogenic massive sulphides. It was last updated on 2026-05-05.

Use Cases

• Modeling paleogeographic zonation based on descriptions of shelf carbonates, rift facies, and back-arc basins.
• Identifying potential mineral deposit locations based on described unconformities, karst, porous carbonates, and reactivated thrusts.
• Analyzing structural controls on mineralization based on descriptions of inverted listric faults and shear zones.
• Correlating granitoid emplacement with tectonic phases based on described syntectonic and post-tectonic intrusions.

Strengths

• Description provides a specific temporal range for sedimentation: from about 540 Ma to at least 510 Ma.
• Identifies distinct geological phases, such as thick rift sedimentation in the Kanmantoo Trough from 526 Ma.
• Mentions specific mineral deposit types and their geological associations, such as Mississippi Valley-type and volcanogenic massive sulphides.

Limitations

• Column-level documentation is absent; field semantics must be inferred after download.
• Row count is unknown, which may limit suitability assessment.
• Description metadata is limited; actual data quality requires manual inspection after download.

Provenance

Source

Australian Ocean Data Network

Time Range

About 540 to at least 510 million years ago (Cambrian period)

Freshness

Last updated 2026-05-05 00:31:29.796735; freshness should be verified.

Geography

Stansbury Basin, Kanmantoo Trough, South Australia