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Predictive Mineralogy

Possible unrecorded species at Gold Hill Mine, Gold Hill, Gold Hill Mining District (Clifton Mining District), Tooele County, Utah, USA

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
SmithsoniteZnCO399.22%Arsentsumebite (56.10 %), Goldhillite (57.14 %), Hemimorphite (55.59 %), Juanitaite (50.00 %), Tsumcorite (60.00 %), Zincolivenite (53.66 %)
PharmacosideriteKFe3+4(AsO4)3(OH)4 路 6-7H2O97.55%Arthurite (61.54 %), Ceruleite (50.00 %), Natropharmacosiderite (72.22 %), Tsumcorite (54.29 %)
PyromorphitePb5(PO4)3Cl89.38%Gartrellite (53.06 %), Leadhillite (53.42 %), Tsumcorite (51.43 %)
SulphurS886.87%Dietrichite (66.67 %), Metavoltine (60.64 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)686.14%Goldhillite (71.43 %), Philipsburgite (51.52 %)
MagnetiteFe2+Fe3+2O480.27%Actinolite (53.38 %), Andradite (57.68 %)
BismuthBi79.58%Bismite (59.17 %), Ferrisymplesite (50.00 %)
Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)78.92%Clinozoisite (56.31 %), Zoisite (51.75 %)
DolomiteCaMg(CO3)278.26%Gilmarite (50.00 %), K枚ttigite (56.52 %)
LangiteCu4(SO4)(OH)6 路 2H2O77.50%Parnauite (53.60 %), Philipsburgite (51.52 %)
MarcasiteFeS266.66%Dietrichite (66.67 %)
HydrozinciteZn5(CO3)2(OH)657.14%Goldhillite (57.14 %)
TheisiteCu5Zn5(AsO4,SbO4)2(OH)1457.14%Goldhillite (57.14 %)
ChalcanthiteCuSO4 路 5H2O55.55%Dietrichite (55.56 %)
MuscoviteKAl2(AlSi3O10)(OH)255.55%Dietrichite (55.56 %)
PseudomalachiteCu5(PO4)2(OH)454.54%Philipsburgite (54.55 %)
KaoliniteAl2(Si2O5)(OH)454.28%Tsumcorite (54.29 %)
UraniniteUO253.70%Metazeunerite (53.70 %)
HalotrichiteFeAl2(SO4)4 路 22H2O53.19%Metavoltine (53.19 %)
FluoriteCaF250.81%Kettnerite (50.82 %)
ParasymplesiteFe2+3(AsO4)2 路 8H2O50.00%Ferrisymplesite (50.00 %)
EnargiteCu3AsS450.00%Juanitaite (50.00 %)
PreisingeriteBi3(AsO4)2O(OH)50.00%Juanitaite (50.00 %)
ErythriteCo3(AsO4)2 路 8H2O43.33%Ferrisymplesite (54.17 %)

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
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Halloysite
452
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]322
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Aikinite, Gilmarite
233
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite, Wulfenite
212
47g : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
105
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hetaerolite
100
47b : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]42
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]28
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)20
50 : Coal and/or oil shale minerals18
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)15
54 : Coal and other mine fire minerals (see also #51 and #56)15
37 : Layered igneous intrusions and related PGE minerals14
56 : Slag and smelter minerals (see also #51 and #55)12
47e : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]12