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- W2017679937 abstract "SUMMARY Related sequences of Holocene fluvial tufa deposits occur in two north Derbyshire valleys. The Lathkill deposits extend, with a break, back into the Devensian and are continuing growth at the present. The Flandrian Wye valley tufas were extinguished historically by pollution and siliciclastic input. A three-dimensional facies framework has been constructed from subsurface data provided by percussion auger sampling and resistivity surveying. Phytoherm barriers are dominated by mosses and semi-aquatic plants heavily encrusted with isopachous sparry calcite fringe cements and lesser developments of micrite fringe cements. The pools and ponded areas upstream of the barriers are dominated by phytoclastic wackestones and cyanoliths (oncoids). Palaeoenvironmental reconstruction indicates that both of the successions are part of a formerly extensive barrage tufa system comparable in type with the Plitvice systems of Croatia. It is suggested that the older Lathkill tufas were deposited under warmer, interglacial conditions." @default.
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- W2017679937 date "1993-05-01" @default.
- W2017679937 modified "2023-10-18" @default.
- W2017679937 title "Sedimentology of the late Quaternary barrage tufas in the Wye and Lathkill valleys, north Derbyshire" @default.
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- W2017679937 doi "https://doi.org/10.1144/pygs.49.3.197" @default.
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