Intergranular aragonite cement as evidence for widespread cryogenic brine formation during Quaternary glaciation in the McMurdo Sound region, Antarctica
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DOI: 10.1016/j.gca.2019.10.027
Abstract: Abstract Briny groundwater is present below the extremely cold and dry surface of the McMurdo Dry Valleys and below the seafloor of the adjacent McMurdo Sound in Antarctica. The lack of reliable groundwater samples in… read more here.
Keywords: cryogenic brine; aragonite cement; mcmurdo sound;