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- W2040474764 abstract "An investigation has been made of the hydrochemistry of the five thermal springs at Matlock Bath and the geochemistry of the associated travertines. The thermal waters are shown to have a common source and originate from precipitation which has equilibrated with a soil atmosphere which has descended through Carboniferous Limestone at a depth probably no greater than 0.5 km. The springs issue below a basalt lava at Matlock Bath at 20°C. Two springs deposit travertine (calcareous tufa) which covers an area of about 6 ha. The travertines consist of low magnesian calcite but with high levels of Sr, Pb and Zn . Their δ13C and δ18O values indicate deposition at or close to isotopic equilibrium with the springwater and confirm a soil-origin of the CO2 in the percolation water. The travertines form around the moss Cratoneuron commutatum which provides an open framework and is ultimately cemented with microspar to form a tough low-porosity deposit. Inactive travertines at the New Bath contain molluscan and pollen assemblages suggesting an open nitrophile woodland environment probably of Atlantic age or later." @default.
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- W2040474764 date "1999-01-01" @default.
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- W2040474764 title "The origin and development of the travertines and associated thermal waters at Matlock Bath, Derbyshire" @default.
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- W2040474764 doi "https://doi.org/10.1016/s0016-7878(99)80072-8" @default.
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