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Predictive Mineralogy

Possible unrecorded species at Tonopah-Belmont Mine, Belmont Mountain, Tonopah, Osborn Mining District, Maricopa County, Arizona, 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
PyromorphitePb5(PO4)3Cl99.82%Bechererite (78.95 %), Leadhillite (53.42 %), Munakataite (68.97 %), Phosphohedyphane (61.96 %), Schmiederite (57.14 %), Vauquelinite (64.38 %)
CupriteCu2O99.55%Bechererite (52.63 %), Botallackite (50.88 %), Cumengeite (55.36 %), Gerhardtite (64.29 %), Schmiederite (64.29 %), Shannonite (66.67 %)
AtacamiteCu2(OH)3Cl92.41%Clinoatacamite (60.71 %), Cumengeite (53.57 %), Paratacamite (58.42 %)
CopperCu79.69%Bechererite (52.63 %), Gerhardtite (57.14 %)
AragoniteCaCO379.62%Paralaurionite (59.26 %), Schmiederite (50.00 %)
DuftitePbCu(AsO4)(OH)79.61%Arsendescloizite (53.57 %), Arsentsumebite (56.10 %)
HydrocerussitePb3(CO3)2(OH)278.60%Paralaurionite (51.85 %), Shannonite (55.56 %)
FluoriteCaF277.77%Murdochite (50.00 %), Shannonite (55.56 %)
BayldonitePbCu3(AsO4)2(OH)260.97%Arsentsumebite (60.98 %)
OliveniteCu2(AsO4)(OH)58.53%Arsentsumebite (58.54 %)
LangiteCu4(SO4)(OH)6 · 2H2O57.89%Bechererite (57.89 %)
Schulenbergite(Cu,Zn)7(SO4)2(OH)10 · 3H2O57.89%Bechererite (57.89 %)
SusannitePb4(CO3)2(SO4)(OH)257.89%Bechererite (57.89 %)
RedgilliteCu6(SO4)(OH)10 · H2O57.89%Bechererite (57.89 %)
LaurionitePbCl(OH)55.55%Paralaurionite (55.56 %)
ConnelliteCu19(SO4)(OH)32Cl4 · 3H2O54.38%Botallackite (54.39 %)
DolomiteCaMg(CO3)253.57%Arsendescloizite (53.57 %)
PyrolusiteMn4+O252.33%Cryptomelane (52.34 %)
MuscoviteKAl2(AlSi3O10)(OH)251.80%Kaolinite (51.81 %)
AcanthiteAg2S51.72%Munakataite (51.72 %)
BeudantitePbFe3(AsO4)(SO4)(OH)651.21%Arsentsumebite (51.22 %)
BorniteCu5FeS450.00%Schmiederite (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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Creaseyite
234
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
144
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
144
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
137
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Ashburtonite
100
56 : Slag and smelter minerals (see also #51 and #55)36
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]32
50 : Coal and/or oil shale minerals27
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]27
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]25
54 : Coal and other mine fire minerals (see also #51 and #56)23
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits19
55 : Anthropogenic mine minerals19
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]14
52 : Guano- and urine-derived minerals12