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Predictive Mineralogy

Possible unrecorded species at Fischbacher Werk Mine, Niederfischbach, Kirchen (Sieg), Altenkirchen, 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
PyrrhotiteFe1-xS99.96%Breithauptite (67.33 %), Cubanite (81.53 %), Gersdorffite (51.37 %), Glaucodot (60.12 %), Nisbite (85.19 %), Polydymite (51.92 %), Ullmannite (59.50 %)
SmithsoniteZnCO399.61%Aurichalcite (54.58 %), Hydrozincite (62.08 %), Namuwite (63.01 %), Ramsbeckite (68.42 %), Rosasite (57.69 %), Schulenbergite (55.35 %)
HemimorphiteZn4Si2O7(OH)2 · H2O99.26%Aurichalcite (50.47 %), Hydrozincite (52.67 %), Namuwite (50.68 %), Ramsbeckite (59.21 %), Rosasite (63.74 %), Tsumebite (56.76 %)
HematiteFe2O396.96%Cobaltkoritnigite (52.94 %), Lepidocrocite (55.13 %), Penroseite (68.75 %), Tsumebite (54.05 %)
SerpieriteCa(Cu,Zn)4(SO4)2(OH)6 · 3H2O94.76%Namuwite (67.12 %), Ramsbeckite (53.95 %), Schulenbergite (65.41 %)
SkutteruditeCoAs381.59%Cobaltkoritnigite (55.88 %), Safflorite (58.29 %)
ClausthalitePbSe81.25%Penroseite (81.25 %)
MagnetiteFe2+Fe3+2O478.89%Cubanite (57.24 %), Polydymite (50.64 %)
StibniteSb2S378.50%Valentinite (78.50 %)
BaryteBaSO477.78%Namuwite (50.68 %), Penroseite (50.00 %), Pyrostilpnite (51.04 %), Ramsbeckite (50.00 %), Tsumebite (54.05 %)
BismuthiniteBi2S368.91%Gladite (68.92 %)
GudmunditeFeSbS62.96%Nisbite (62.96 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 162.16%Tsumebite (62.16 %)
CobaltiteCoAsS58.92%Glaucodot (58.93 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
ArsenoliteAs2O350.00%Cobaltkoritnigite (50.00 %)
GoldAu45.00%Penroseite (56.25 %)
WulfenitePb(MoO4)43.24%Tsumebite (54.05 %)

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: Bournonite, Freibergite Subgroup, Gladite, Glaucodot, Nisbite, Penroseite, etc.
1,271
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]118
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

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

Unique: Hörnesite
100
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]56
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]32
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]29
56 : Slag and smelter minerals (see also #51 and #55)26
37 : Layered igneous intrusions and related PGE minerals26
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]21
55 : Anthropogenic mine minerals20
49 : Oxic cellular biomineralization (see also #44)14
6 : Secondary asteroid phases13