Lakes in the Salt Creek area of the Coorong region, South Australia, contain a
diverse suite of Holocene carbonates including aragonite, calcite, Mg-calcite,
magnesite, hydromagnesite, and dolomite. Dolomite has been the main mineral of
concern in previous geological studies of this area, yet it makes up no more
than 5% of the carbonate minerals forming surficial deposits across the coastal
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