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Predictive Mineralogy

Possible unrecorded species at Kanmantoo Mine (Kanmantoo West; Kanmantoo North), Kanmantoo, South Mt Lofty Ranges (Adelaide Hills), Mt Lofty Ranges, South Australia, Australia

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
CalciteCaCO395.68%Digenite (52.28 %), Epidote (51.60 %), Laitakarite (52.50 %), Marcasite (60.67 %)
ArsenopyriteFeAsS70.28%Joséite-B (73.00 %), Laitakarite (55.00 %)
AlbiteNa(AlSi3O8)51.77%Monazite-(Ce) (51.78 %)
ZirconZr(SiO4)43.98%Monazite-(Ce) (54.99 %)

Key: Mineral matches key element mineralogy of deposit Key element(s) in mineral not listed for deposit (-20% score)


Predicting paragenetic modes of deposit

Green indicates almost certain match based on minerals unique to a certain deposit type. Yellow indicates a possibly poor match, but should not be entirely discounted. Scores > 100 indicate strong confidence.

Paragenetic ModeScore
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Laitakarite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)22
34 : Complex granite pegmatites14
26 : Hadean detrital minerals12
31 : Thermally altered carbonate, phosphate, and iron formations12
6 : Secondary asteroid phases10
53 : Other minerals with taphonomic origins7
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]6
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]6
50 : Coal and/or oil shale minerals5
54 : Coal and other mine fire minerals (see also #51 and #56)5