Mineral sands occurrences in the Murray Basin, southeastern Australia
Mineral sands occurrences in the Murray Basin, southeastern Australia
Economic Geology and the Bulletin of the Society of Economic Geologists (August 2000) 95 (5): 1107-1128
- Australasia
- Australia
- beach placers
- Cenozoic
- climatic controls
- concentration
- fluvial environment
- geomorphologic controls
- heavy mineral deposits
- mineral deposits, genesis
- Murray Basin
- Neogene
- New South Wales Australia
- paleoclimatology
- paleogeography
- placers
- Pliocene
- production
- sands
- sea-level changes
- South Australia
- Tertiary
- tonnage
- zircon deposits
- southeastern Australia
- ilmenite deposits
- Loxton-Parilla Sands
- rutile deposits
The Murray Basin is proving to be a major mineral sand province that eventually will replace Australia's east and west coasts in production of rutile, zircon and ilmenite. Concentrations of relatively coarse-grained heavy mineral are found as beach placers in Pliocene sands of the upper Murray Basin. Typically, they are ilmenite-rich, with 30-40% rutile and zircon. They occur as single or multiple, stacked strandline deposits often > 10 m thick, have mineral grades that exceed 20% in places, are several hundred m wide and 10-25 km long, some containing several Mt of heavy minerals. The rutile and zircon are comparable in grain size and quality to minerals traditionally mined in Australia. The total, coarse-grained mineral sand resources in the Murray Basin are conservatively estimated to be over 50 Mt. The geology and geomorphology of these placer deposits are discussed.