Abstract
Aragonite has deposited from waters discharged from Broadlands geothermal drillhole, Br6. Waters from the drillhole, in contrast with others from the geothermal field, are highly supersaturated with CaCO3 and contain relatively high concentrations of Mg2+, Ca2+, Sr2+ and HCO3-. The formation of aragonite instead of calcite results from the rapid precipitation rate and the stabilising effect of the Ba2+, Sr2+, and possibly Mg2+ on the orthorhombic structure.

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