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Predictive Mineralogy

Possible unrecorded species at Mt Painter area, Arkaroola Region (Arkaroola Wilderness Sanctuary; Arkaroola Station), North Flinders Ranges, Flinders 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
GalenaPbS99.78%Cerussite (83.05 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Dewindtite (50.00 %), Françoisite-(Nd) (66.67 %), Witherite (57.59 %)
AlbiteNa(AlSi3O8)97.47%Elbaite (66.61 %), Ishikawaite (64.29 %), Microcline (56.11 %), Monazite-(Ce) (51.78 %)
BerylBe3Al2(Si6O18)83.51%Elbaite (60.85 %), Magnesiotaaffeite-2N’2S (57.89 %)
SphaleriteZnS73.96%Cerussite (56.70 %), Chalcopyrite (50.66 %), Covellite (64.68 %)
Uranopilite(UO2)6(SO4)O2(OH)6 · 14H2O66.66%Françoisite-(Nd) (66.67 %)
ChrysoberylBeAl2O463.15%Magnesiotaaffeite-2N’2S (63.16 %)
Columbite-(Fe)Fe2+Nb2O653.57%Ishikawaite (53.57 %)
GypsumCaSO4 · 2H2O50.28%Sulphur (50.28 %)
CassiteriteSnO242.10%Magnesiotaaffeite-2N’2S (52.63 %)

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
34 : Complex granite pegmatites

Unique: Ishikawaite
131
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]113
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Davidite-(La)
100
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]97
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]34
26 : Hadean detrital minerals29
31 : Thermally altered carbonate, phosphate, and iron formations18
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]17
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)13
48 : Soil leaching zone minerals12
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits12
27 : Radioactive decay; auto-oxidation10