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Predictive Mineralogy

Possible unrecorded species at Silberbrünnle Mine, Gengenbach, Gengenbach, 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
ArsenopyriteFeAsS99.99%Carminite (53.49 %), Dussertite (50.00 %), Gustavite (56.59 %), Matildite (55.24 %), Mawbyite (54.17 %), Philipsbornite (58.06 %), Pitticite (66.67 %), Schapbachite (52.00 %), Scorodite (74.10 %), Segnitite (57.06 %), Thometzekite (69.23 %), Waylandite (50.00 %)
FluoriteCaF298.72%Agardite-(Ce) (62.50 %), Bastnäsite-(Ce) (57.77 %), Rhabdophane-(Ce) (55.42 %), Synchysite-(Ce) (60.92 %), Thometzekite (53.85 %)
AlbiteNa(AlSi3O8)98.30%Bastnäsite-(Ce) (59.33 %), Chernovite-(Y) (52.63 %), Monazite-(Ce) (51.78 %), Rhabdophane-(Ce) (54.22 %), Synchysite-(Ce) (60.21 %)
SmithsoniteZnCO397.80%Arsendescloizite (71.43 %), Mawbyite (50.00 %), Thometzekite (61.54 %), Tsumcorite (60.00 %)
BismuthiniteBi2S397.17%Berryite (57.14 %), Bismutoferrite (52.63 %), Emplectite (57.24 %), Gustavite (67.44 %)
SideriteFeCO394.82%Agardite-(Ce) (52.08 %), Delafossite (52.66 %), Diadochite (50.60 %), Thometzekite (53.85 %)
BismuthBi93.34%Bismutoferrite (66.67 %), Eulytine (54.76 %), Waylandite (55.88 %)
PharmacosideriteKFe3+4(AsO4)3(OH)4 · 6-7H2O92.08%Mawbyite (62.50 %), Thometzekite (53.85 %), Tsumcorite (54.29 %)
LeadhillitePb4(CO3)2(SO4)(OH)289.51%Elyite (51.61 %), Susannite (53.04 %), Thometzekite (53.85 %)
HemimorphiteZn4Si2O7(OH)2 · H2O83.22%Arsendescloizite (64.29 %), Susannite (53.04 %)
MagnetiteFe2+Fe3+2O482.56%Andradite (57.68 %), Bastnäsite-(Ce) (58.81 %)
ZirconZr(SiO4)76.99%Arsenoflorencite-(Ce) (50.00 %), Bastnäsite-(Ce) (66.06 %), Chernovite-(Y) (50.88 %), Monazite-(Ce) (54.99 %)
MicroclineK(AlSi3O8)76.83%Bastnäsite-(Ce) (50.78 %), Rhabdophane-(La) (52.94 %)
RutileTiO264.84%Arsenoflorencite-(Ce) (60.00 %), Chernovite-(Y) (52.63 %)
AnataseTiO260.56%Arsenoflorencite-(Ce) (50.00 %), Synchysite-(Ce) (51.41 %)
GoldAu60.00%Berryite (50.00 %), Tripuhyite (50.00 %)
AikinitePbCuBiS357.14%Berryite (57.14 %)
Xenotime-(Y)Y(PO4)54.38%Chernovite-(Y) (54.39 %)
PyrrhotiteFe1-xS54.26%Gustavite (54.26 %)
ArsentsumebitePb2Cu(AsO4)(SO4)(OH)53.84%Thometzekite (53.85 %)
ChalcanthiteCuSO4 · 5H2O53.84%Thometzekite (53.85 %)
HidalgoitePbAl3(AsO4)(SO4)(OH)653.84%Thometzekite (53.85 %)
Lepidocrociteγ-Fe3+O(OH)53.84%Thometzekite (53.85 %)
UraniniteUO253.70%Metazeunerite (53.70 %)
StibniteSb2S353.57%Tripuhyite (53.57 %)
ChlorargyriteAgCl53.06%Gartrellite (53.06 %)
Agardite-(Y)YCu6(AsO4)3(OH)6 · 3H2O52.63%Agardite-(Nd) (52.63 %)
LanarkitePb2(SO4)O51.61%Elyite (51.61 %)
RhodochrositeMnCO351.25%Hausmannite (51.25 %)
TyroliteCa2Cu9(AsO4)4(CO3)(OH)8 · 11H2O50.40%Parnauite (50.40 %)
ErythriteCo3(AsO4)2 · 8H2O46.21%Annabergite (57.77 %)
TitaniteCaTi(SiO4)O40.00%Synchysite-(Ce) (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: Berryite, Emplectite, Enargite, Eulytine, Matildite, Pyrargyrite, etc.
652
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]352
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]292
34 : Complex granite pegmatites

Unique: Rhabdophane-(La), Rhabdophane-(Nd)
190
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Gustavite, Luzonite
178
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]147
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
141
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hausmannite
100
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]18
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)18
35 : Ultra-alkali and agpaitic igneous rocks18
49 : Oxic cellular biomineralization (see also #44)16
55 : Anthropogenic mine minerals14
56 : Slag and smelter minerals (see also #51 and #55)14
26 : Hadean detrital minerals13