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Murray Basin
Testing the Gippsland Basin zonation in northern Australia: palynostratigraphical analysis of a 23 Ma 40 Ar/ 39 Ar dated claystone from Toowoomba, southeast Queensland
A comparative study of in-river geophysical techniques to define variations in riverbed salt load and aid managing river salinization
Baseline geochemical survey of the Riverina region of New South Wales and Victoria, Australia: concentrations and distributions of As, Ba, Br, Cd, Co, Cr, F, Ga, Mo, Sb, U and V compared to national and international guidelines
An evaluation of methods for imputation of missing trace element data in groundwaters
Brachiopods in Epeiric Seas as Monitors of Secular Changes in Ocean Chemistry: A Miocene Example from the Murray Basin, South Australia
75th Anniversary: The historical development of the magnetic method in exploration
Behaviour of impurity elements during the weathering of ilmenite
Quantitative Heavy-Mineral Analysis of a Pliocene Beach Placer Deposit in Southeastern Australia Using the AutoGeoSEM
Compositional and textural variation in detrital chrome-spinels from the Murray Basin, southeastern Australia
Paleoenvironmental Significance of Celleporaria (Bryozoa) from Modern and Tertiary Cool-water Carbonates of Southern Australia
Deepening-Upward Subtidal Cycles, Murray Basin, South Australia
Hydroxylian pseudorutile derived from picroilmenite in the Murray Basin, southeastern Australia
Changing Pliocene Sea Levels and the Formation of Heavy Minerals Beach Placers in the Murray Basin, Southeastern Australia
Origin and Timing of the Miocene-Pliocene Unconformity in Southeast Australia
A Review of Tertiary Brown Coal Deposits in Australia: Their Depositional Factors and Eustatic Correlations
Mineral Sands Occurrences in the Murray Basin, Southeastern Australia
Palynostratigraphy of the Murray Basin, inland southeastern Australia
Selwynite, NaK(Be,Al)Zr 2 (PO 4 ) 4 .2H 2 O, a new gainesite-like mineral from Wycheproof, Victoria, Australia
Groundwater discharge complexes, locally known as boinkas, are a distinctive feature of the Mallee region, the western sector of the Murray Basin (300,000 km 2 ) in southeast Australia. The discharge complexes are nested, with modern playas (salinas) set in late Pleistocene playa sediments and associated aeolian deposits. Playa evolution started with the onset of aridity in the mid-Pleistocene. In the Murray Basin, groundwater discharges, and has discharged in the past, to topo-graphically low parts of the landscape,, including the Murray River itself. The fundamental control on the distribution of the discharge complexes is the presence of subsurface permeability barriers, which are tectonically or stratigraphically controlled, and which disrupt lateral groundwater flow. With the general absence of surface drainage in the Mallee region, the location of the topographic lows is probably influenced by differential compaction of sediments. Within the modern salinas, brine is generated by evaporative concentration and resolution of salts. The structure of some of the investigated brine pools suggests that density instability leads to brine fingering, sinking, and mixing with regional groundwaters. This process is facilitated by more permeable sediments. “Fossil” brines generated by the late Pleistocene playas can be identified and have contributed to the salinity of the regional unconfined aquifer. Brine pools have migrated in time and space in response to climatic change. This has practical implications for the long-term containment of saline wastewaters, which is a serious problem in the Murray Basin.