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Predictive Mineralogy

Possible unrecorded species at Bad Ems-Nassau, Rhein-Lahn-Kreis, Rhineland-Palatinate, Germany

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
BaryteBaSO499.99%Arsenogorceixite (70.59 %), Arsentsumebite (68.29 %), Bayldonite (55.28 %), Beaverite-(Cu) (55.09 %), Brianyoungite (50.54 %), Duftite (57.09 %), Dundasite (58.56 %), Glaucocerinite (57.14 %), Hinsdalite (53.76 %), Koritnigite (63.64 %), Köttigite (60.87 %), Ktenasite (56.52 %), Namuwite (50.68 %), Ramsbeckite (50.00 %), Richelsdorfite (63.24 %), Schultenite (61.54 %), Strashimirite (65.22 %), Tsumcorite (54.29 %), Tyrolite (52.96 %)
CovelliteCuS99.99%Arsentsumebite (60.98 %), Bayldonite (51.26 %), Beaverite-(Cu) (52.10 %), Caledonite (50.12 %), Delafossite (58.58 %), Glaucocerinite (57.14 %), Ktenasite (67.39 %), Namuwite (57.53 %), Philipsbornite (50.00 %), Posnjakite (54.49 %), Ramsbeckite (59.21 %), Richelsdorfite (51.47 %), Schulenbergite (57.23 %), Schultenite (56.41 %), Serpierite (52.17 %), Stranskiite (62.50 %), Susannite (56.52 %), Tsumcorite (54.29 %), Wroewolfeite (56.60 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)699.81%Brianyoungite (50.54 %), Glaucocerinite (71.43 %), Ktenasite (50.00 %), Namuwite (60.27 %), Ramsbeckite (65.79 %), Rosasite (59.34 %), Schulenbergite (52.83 %)
SulphurS899.69%Koritnigite (63.64 %), Namuwite (54.79 %), Quenstedtite (57.89 %), Ramsbeckite (53.95 %), Schultenite (61.54 %), Stranskiite (75.00 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 199.23%Arsentsumebite (68.29 %), Duftite (51.18 %), Koritnigite (54.55 %), Pseudomalachite (50.70 %), Stranskiite (50.00 %), Strashimirite (55.65 %)
SilverAg98.00%Acanthite (50.32 %), Breithauptite (50.99 %), Köttigite (55.07 %), Schultenite (51.28 %), Stranskiite (62.50 %)
AdamiteZn2(AsO4)(OH)97.63%Austinite (59.52 %), Koritnigite (54.55 %), Stranskiite (62.50 %), Tsumcorite (65.71 %)
CinnabarHgS95.05%Mercury (80.24 %), Stranskiite (75.00 %)
MarcasiteFeS294.09%Honessite (56.67 %), Koritnigite (63.64 %), Stranskiite (62.50 %)
ConichalciteCaCu(AsO4)(OH)80.95%Austinite (58.33 %), Tsumcorite (54.29 %)
PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2O79.22%Koritnigite (54.55 %), Tsumcorite (54.29 %)
MagnetiteFe2+Fe3+2O468.10%Valleriite (68.10 %)
StrengiteFePO4 · 2H2O62.55%Beraunite (62.56 %)
CacoxeniteFe3+24AlO6(PO4)17(OH)12 · 75H2O62.08%Beraunite (62.09 %)
RockbridgeiteFe2+Fe3+4(PO4)3(OH)559.24%Beraunite (59.24 %)
CubaniteCuFe2S356.27%Valleriite (56.27 %)
LavendulanNaCaCu5(AsO4)4Cl · 5H2O54.54%Koritnigite (54.55 %)
ChlorargyriteAgCl53.84%Bromargyrite (53.85 %)
CyanotrichiteCu4Al2(SO4)(OH)12 · 2H2O52.38%Glaucocerinite (52.38 %)
WoodwarditeCu1-xAlx(OH)2(SO4)x/2 · nH2O52.38%Glaucocerinite (52.38 %)
HydrocerussitePb3(CO3)2(OH)251.30%Susannite (51.30 %)
EnargiteCu3AsS450.00%Stranskiite (50.00 %)
ParnauiteCu9(AsO4)2(SO4)(OH)10 · 7H2O50.00%Stranskiite (50.00 %)
GreenockiteCdS40.00%Stranskiite (50.00 %)
WulfenitePb(MoO4)40.00%Stranskiite (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]379
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Bournonite, Pyrargyrite, Ullmannite
374
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Bromargyrite, Iodargyrite
216
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
211
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]190
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hetaerolite
120
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]119
48 : Soil leaching zone minerals

Unique: Gibbsite
101
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
100
37 : Layered igneous intrusions and related PGE minerals39
56 : Slag and smelter minerals (see also #51 and #55)30
55 : Anthropogenic mine minerals29
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]28
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]18
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]15
49 : Oxic cellular biomineralization (see also #44)14