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Predictive Mineralogy

Possible unrecorded species at Hilfe Gottes Mine, Stammelbach valley, Schiltach, Rottweil, 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
MalachiteCu2(CO3)(OH)299.99%Arseniosiderite (53.98 %), Asbolane (51.19 %), Bariopharmacosiderite (65.05 %), Brochantite (75.59 %), Chrysocolla (74.38 %), Covellite (54.66 %), Cuprite (79.07 %), Emplectite (53.79 %), Erythrite (51.09 %), Langite (85.29 %), Lavendulan (70.18 %), Mixite (70.31 %), Olivenite (76.60 %), Pharmacolite (50.00 %), Zeunerite (51.16 %)
AzuriteCu3(CO3)2(OH)299.23%Bariopharmacosiderite (54.30 %), Cuprite (51.54 %), Langite (53.49 %), Lavendulan (52.05 %), Mixite (54.17 %), Olivenite (66.38 %)
SilverAg96.08%Pharmacolite (54.31 %), Proustite (56.73 %), Safflorite (59.63 %), Skutterudite (50.92 %)
ArsenopyriteFeAsS95.49%Arsenic (53.29 %), Arsenolite (55.13 %), Hörnesite (52.00 %), Pharmacolite (55.17 %)
Goethiteα-Fe3+O(OH)94.62%Arseniosiderite (52.65 %), Bariopharmacosiderite (52.69 %), Langite (50.97 %), Mixite (51.04 %)
DolomiteCaMg(CO3)293.69%Hörnesite (63.20 %), Pharmacolite (61.21 %), Picropharmacolite (55.83 %)
GalenaPbS79.99%Arsenic (59.62 %), Arseniosiderite (52.21 %), Arsenolite (53.61 %), Bariopharmacosiderite (53.23 %), Bismuth (51.78 %), Bismuthinite (57.89 %), Brochantite (55.97 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Emplectite (61.38 %), Erythrite (53.28 %), Hörnesite (58.40 %), Langite (63.00 %), Lavendulan (54.39 %), Marcasite (58.73 %), Metaheinrichite (54.55 %), Olivenite (50.95 %), Pharmacolite (59.48 %), Proustite (67.15 %), Pyrargyrite (72.03 %), Safflorite (59.36 %), Skutterudite (51.58 %), Sphalerite (74.68 %), Wittichenite (68.22 %)
ChalcociteCu2S78.21%Covellite (50.30 %), Wittichenite (56.16 %)
AcanthiteAg2S78.02%Proustite (55.52 %), Pyrargyrite (50.61 %)
MetazeuneriteCu(UO2)2(AsO4)2 · 8H2O68.18%Metaheinrichite (68.18 %)
MuscoviteKAl2(AlSi3O10)(OH)262.63%Schorl (62.64 %)
OrpimentAs2S358.52%Realgar (58.53 %)
ScoroditeFe3+AsO4 · 2H2O57.52%Arseniosiderite (57.52 %)
GoldAu43.17%Wittichenite (53.97 %)
CerussitePbCO343.15%Langite (53.94 %)

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, Emplectite, Proustite, Pyrargyrite, Safflorite, Wittichenite
607
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite
106
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]79
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]74
53 : Other minerals with taphonomic origins15
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)14
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]11
55 : Anthropogenic mine minerals9
50 : Coal and/or oil shale minerals8
54 : Coal and other mine fire minerals (see also #51 and #56)8
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]7
34 : Complex granite pegmatites7