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Predictive Mineralogy

Possible unrecorded species at Kalgoorlie-Boulder, Kalgoorlie-Boulder Shire, Western 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
AcanthiteAg2S99.80%Aguilarite (68.81 %), Jalpaite (75.54 %), Marrite (66.67 %), Proustite (55.52 %), Pyrargyrite (50.61 %), Pyrostilpnite (64.58 %)
BismuthiniteBi2S399.75%Cosalite (58.38 %), Felbertalite (50.00 %), Junoite (65.00 %), Krupkaite (70.10 %), Nuffieldite (57.89 %), Pekoite (73.33 %)
BismuthBi97.29%Felbertalite (50.00 %), Junoite (50.00 %), Krupkaite (50.52 %), Nuffieldite (55.26 %), Pekoite (51.11 %)
TellurobismuthiteBi2Te393.14%Frohbergite (57.14 %), Mattagamite (66.67 %), Montbrayite (52.00 %)
KlockmanniteCuSe82.99%Eucairite (59.68 %), Umangite (57.83 %)
CerussitePbCO366.66%Marrite (66.67 %)
FluoriteCaF266.66%Marrite (66.67 %)
PyrolusiteMn4+O263.98%Manganite (63.98 %)
GladitePbCuBi5S955.55%Pekoite (55.56 %)
StephaniteAg5SbS453.12%Pyrostilpnite (53.13 %)
Goldfieldite(Cu42)(Cu4Cu+2)Te4S12S51.72%Kostovite (51.72 %)
WitticheniteCu3BiS350.00%Felbertalite (50.00 %)
LillianitePb3-2xAgxBi2+xS650.00%Junoite (50.00 %)
MolybdeniteMoS244.44%Mattagamite (55.56 %)
UraniniteUO240.00%Nolanite (50.00 %)

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: Aguilarite, Aikinite, Aleksite, Arsenic, Boulangerite, Bournonite, etc.
4,429
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Halloysite
136
6 : Secondary asteroid phases

Unique: Breunnerite
124
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Siegenite
103
48 : Soil leaching zone minerals

Unique: Gibbsite
101
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
100
37 : Layered igneous intrusions and related PGE minerals41
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)28
31 : Thermally altered carbonate, phosphate, and iron formations27
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)26
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]25
46 : Near-surface hydrothermal alteration of minerals (see also #22)17
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]14
50 : Coal and/or oil shale minerals12
26 : Hadean detrital minerals12
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]11