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Predictive Mineralogy

Possible unrecorded species at Michael Mine, Weiler, Seelbach, Seelbach, Ortenaukreis, Freiburg Region, Baden-Württemberg, 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
GypsumCaSO4 · 2H2O99.99%Arsendescloizite (50.00 %), Bariopharmacoalumite (50.00 %), Halotrichite (61.51 %), Heinrichite (61.90 %), Hidalgoite (54.55 %), Köttigite (57.97 %), Metanováčekite (53.33 %), Nováčekite (83.33 %), Schultenite (64.10 %), Sulphur (50.28 %), Szomolnokite (65.22 %), Tsumcorite (57.14 %)
ArsenopyriteFeAsS99.99%Arsenic (53.29 %), Arsenogorceixite (58.82 %), Arsenolite (55.13 %), Carminite (53.49 %), Gersdorffite (50.38 %), Hügelite (54.55 %), Parasymplesite (55.32 %), Philipsbornite (58.06 %), Pitticite (66.67 %), Schultenite (61.54 %), Segnitite (57.06 %)
ScoroditeFe3+AsO4 · 2H2O99.97%Arseniosiderite (57.52 %), Arsenogorceixite (70.59 %), Carminite (65.12 %), Hidalgoite (50.65 %), Parasymplesite (56.74 %), Philipsbornite (58.06 %), Pitticite (50.67 %), Schultenite (64.10 %), Tsumcorite (65.71 %)
OliveniteCu2(AsO4)(OH)99.66%Arsenogorceixite (58.82 %), Bariopharmacoalumite (66.67 %), Bariopharmacosiderite (51.08 %), Bayldonite (52.26 %), Tsumcorite (71.43 %), Zincolivenite (63.41 %)
UranophaneCa(UO2)2(SiO3OH)2 · 5H2O99.39%Heinrichite (52.38 %), Kasolite (60.18 %), Metanováčekite (56.67 %), Nováčekite (66.67 %), Parsonsite (55.88 %), Widenmannite (50.00 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 191.74%Duftite (51.18 %), Zálesíite (65.35 %), Zincolivenite (51.22 %)
TorberniteCu(UO2)2(PO4)2 · 12H2O86.63%Hügelite (54.55 %), Parsonsite (70.59 %)
PyrargyriteAg3SbS382.02%Proustite (53.45 %), Xanthoconite (61.39 %)
ConichalciteCaCu(AsO4)(OH)80.95%Austinite (58.33 %), Tsumcorite (54.29 %)
MuscoviteKAl2(AlSi3O10)(OH)276.43%Kaolinite (51.81 %), Montmorillonite (51.11 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O69.11%Parsonsite (69.12 %)
FluoriteCaF266.66%Nováčekite (66.67 %)
CornubiteCu5(AsO4)2(OH)466.66%Bariopharmacoalumite (66.67 %)
CornwalliteCu5(AsO4)2(OH)466.66%Bariopharmacoalumite (66.67 %)
Safflorite(Co,Ni,Fe)As263.63%Metaheinrichite (63.64 %)
BoulangeritePb5Sb4S1159.23%Geocronite (59.24 %)
AtacamiteCu2(OH)3Cl58.42%Paratacamite (58.42 %)
ChalcophylliteCu18Al2(AsO4)4(SO4)3(OH)24 · 36H2O58.33%Bariopharmacoalumite (58.33 %)
PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2O54.28%Tsumcorite (54.29 %)
BournonitePbCuSbS353.50%Geocronite (53.50 %)
PyrrhotiteFe1-xS51.36%Gersdorffite (51.37 %)
SideriteFeCO351.28%Schultenite (51.28 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
LavendulanNaCaCu5(AsO4)4Cl · 5H2O50.00%Bariopharmacoalumite (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: Arsenic, Proustite, Xanthoconite
317
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]234
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]227
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
134
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Gratonite
107
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
100
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]35
53 : Other minerals with taphonomic origins19
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]19
49 : Oxic cellular biomineralization (see also #44)15
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)12
37 : Layered igneous intrusions and related PGE minerals11
50 : Coal and/or oil shale minerals11
54 : Coal and other mine fire minerals (see also #51 and #56)11