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Predictive Mineralogy

Possible unrecorded species at Concordia 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
BrochantiteCu4(SO4)(OH)699.89%Caledonite (56.97 %), Langite (72.66 %), Leadhillite (53.77 %), Linarite (54.30 %), Ramsbeckite (80.26 %), Schulenbergite (79.25 %)
GypsumCaSO4 · 2H2O98.80%Bottinoite (50.00 %), Pharmacolite (62.07 %), Ramsbeckite (60.53 %), Schulenbergite (67.92 %), Sulphur (50.28 %)
StibniteSb2S397.09%Plagionite (70.80 %), Semseyite (53.77 %), Valentinite (78.50 %)
SilverAg88.85%Acanthite (50.32 %), Pharmacolite (54.31 %), Skutterudite (50.92 %)
AzuriteCu3(CO3)2(OH)288.73%Cuprite (51.54 %), Langite (53.49 %), Ramsbeckite (50.00 %)
SerpieriteCa(Cu,Zn)4(SO4)2(OH)6 · 3H2O84.06%Ramsbeckite (53.95 %), Schulenbergite (65.41 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)683.86%Ramsbeckite (65.79 %), Schulenbergite (52.83 %)
AragoniteCaCO381.14%Ramsbeckite (55.26 %), Schulenbergite (57.86 %)
HemimorphiteZn4Si2O7(OH)2 · H2O80.69%Hydrozincite (52.67 %), Ramsbeckite (59.21 %)
DolomiteCaMg(CO3)280.60%Bottinoite (50.00 %), Pharmacolite (61.21 %)
MarcasiteFeS278.52%Plagionite (56.64 %), Semseyite (50.47 %)
HematiteFe2O377.95%Lepidocrocite (55.13 %), Pharmacolite (50.86 %)
BaryteBaSO471.45%Pharmacolite (56.90 %), Plagionite (50.44 %), Ramsbeckite (50.00 %)
MilleriteNiS70.00%Bottinoite (70.00 %)
PyrrhotiteFe1-xS59.49%Ullmannite (59.50 %)
PosnjakiteCu4(SO4)(OH)6 · H2O53.94%Ramsbeckite (53.95 %)
ZinkenitePb9Sb22S4253.09%Plagionite (53.10 %)
PicropharmacoliteCa4Mg(AsO4)2(HAsO4)2 · 11H2O52.58%Pharmacolite (52.59 %)
GoldAu42.38%Aikinite (52.99 %)

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: Aikinite, Boulangerite, Bournonite, Plagionite, Semseyite, Ullmannite
536
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]44
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]33
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]13
49 : Oxic cellular biomineralization (see also #44)12
55 : Anthropogenic mine minerals10
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]9
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]7
56 : Slag and smelter minerals (see also #51 and #55)5
57 : Other minerals formed by human processes5
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]4