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or periodical (sea) water afflux, to allow the deposit of a decent amount of gypsum. If there is no (temporary) connection to the sea, the layer would be rather thin. Now you have gypsum, but there is another problem: water is able to solute gypsum without the complicated CO2 stuff wi...

www.showcaves.com/english/explain/Speleology/Gypsum.html

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