Abstract
Summary
Biphosphammite, ammonian
KH2PO4,
syngenite, aphthitalite, monetite, hannayite,
whitloekite, apatite and minor gypsum, taylorite,
brushite, mirabilite, guanine, and unidentified
compounds form crystalline crusts on the walls and
floors of a chamber of Murra-el-elevyn Cave,
Cocklebiddy, Nullarbor Plain, Western Australia.
The minerals are derived from the interaction of
bat urine, droppings, and limestone. Analyses for
CaO, MgO, Na2O,
K2O,
SO3,
P2O5,
CO2,
NH3,
H2O-,
total N, and ignition loss are given. High
K2O and low total N figures
are characteristic of the analyses.
Subject
Geochemistry and Petrology
Cited by
25 articles.
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