Geology Reference
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Fig. 5. Field views of different tufa components at the G¨ ney perched springline tufa site. (a) Encrusted algal mass
associated with macrophyte pieces was enclosed by fine grained detrital tufa layer (upper right corner); (b) The
light-coloured and laminated tufa facies, lower slope, roadside section; (c) Calcified, fragile bryophyte cluster in the
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