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Predictive Mineralogy

Possible unrecorded species at Thann-Guebwiller, Haut-Rhin, Grand Est, France

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
DomeykiteCu3As93.87%Koutekite (71.43 %), Kutinaite (50.00 %), Trigodomeykite (57.14 %)
KasolitePb(UO2)(SiO4) · H2O93.56%Billietite (53.66 %), Sharpite (66.67 %), Wölsendorfite (58.33 %)
BerzelianiteCu2-xSe (x ≈ 0.12)83.10%Klockmannite (53.25 %), Umangite (63.86 %)
BeudantitePbFe3(AsO4)(SO4)(OH)669.38%Gartrellite (69.39 %)
BayldonitePbCu3(AsO4)2(OH)265.30%Gartrellite (65.31 %)
CarminitePbFe3+2(AsO4)2(OH)265.30%Gartrellite (65.31 %)
DuftitePbCu(AsO4)(OH)59.18%Gartrellite (59.18 %)
NickelineNiAs58.25%Nickelskutterudite (58.25 %)
SainfelditeCa5(AsO4)2(AsO3OH)2 · 4H2O54.05%Guérinite (54.05 %)
ChlorargyriteAgCl53.06%Gartrellite (53.06 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O51.51%Torbernite (51.52 %)
RauenthaliteCa3(AsO4)2 · 10H2O51.35%Guérinite (51.35 %)
AdamiteZn2(AsO4)(OH)51.02%Gartrellite (51.02 %)
SerpieriteCa(Cu,Zn)4(SO4)2(OH)6 · 3H2O50.00%Zincrosasite (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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Aikinite, Allargentum, Bournonite, Clausthalite, Cosalite, Dyscrasite, etc.
1,983
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]256
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
178
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]162
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
108
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Fukuchilite
102
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
100
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]44
6 : Secondary asteroid phases33
37 : Layered igneous intrusions and related PGE minerals27
55 : Anthropogenic mine minerals25
53 : Other minerals with taphonomic origins22
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]19
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]18
50 : Coal and/or oil shale minerals17