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Predictive Mineralogy

Possible unrecorded species at Schmitt dolomite quarry, Altenmittlau, Freigericht, Main-Kinzig-Kreis, Darmstadt, Hesse, 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
PyriteFeS299.99%Anglesite (64.19 %), Azurite (58.39 %), Baryte (50.79 %), Brochantite (63.33 %), Calcite (51.16 %), Cerussite (56.77 %), Chalcopyrite (75.16 %), Conichalcite (51.29 %), Cuprite (58.26 %), Dolomite (58.22 %), Duftite (57.87 %), Galena (66.84 %), Hedyphane (56.25 %), Lepidocrocite (71.47 %), Malachite (52.79 %), Mimetite (59.01 %), Minium (50.70 %), Molybdenite (68.29 %), Muscovite (50.01 %), Olivenite (56.33 %), Pyromorphite (55.98 %), Tenorite (59.82 %), Tsumebite (51.35 %), Tyrolite (57.84 %), Zincolivenite (63.41 %)
SphaleriteZnS99.99%Anglesite (64.09 %), Brochantite (50.32 %), Cerussite (56.70 %), Chalcopyrite (50.66 %), Duftite (51.18 %), Galena (65.95 %), Hedyphane (57.81 %), Mimetite (53.11 %), Minium (58.45 %), Pyromorphite (56.90 %), Tsumebite (56.76 %), Zincolivenite (54.88 %)
Goethiteα-Fe3+O(OH)99.33%Duftite (50.39 %), Lepidocrocite (76.37 %), Tangdanite (60.00 %), Tsumebite (70.27 %), Zincolivenite (52.44 %)
HematiteFe2O396.27%Fornacite (51.82 %), Hedyphane (62.50 %), Lepidocrocite (55.13 %), Tsumebite (54.05 %)
HemimorphiteZn4Si2O7(OH)2 · H2O56.75%Tsumebite (56.76 %)
GypsumCaSO4 · 2H2O54.05%Tsumebite (54.05 %)
LinaritePbCu(SO4)(OH)254.05%Tsumebite (54.05 %)
SmithsoniteZnCO353.65%Zincolivenite (53.66 %)
ChalcophylliteCu18Al2(AsO4)4(SO4)3(OH)24 · 36H2O53.33%Tangdanite (53.33 %)
ChalcociteCu2S51.43%Tenorite (51.44 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)651.35%Tsumebite (51.35 %)
CovelliteCuS51.35%Tsumebite (51.35 %)
AdamiteZn2(AsO4)(OH)50.00%Zincolivenite (50.00 %)
SilverAg41.08%Tsumebite (51.35 %)

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

Unique: Wulfenite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]67
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]57
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]14
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]13
53 : Other minerals with taphonomic origins8
50 : Coal and/or oil shale minerals8
54 : Coal and other mine fire minerals (see also #51 and #56)8
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]7
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]6
56 : Slag and smelter minerals (see also #51 and #55)5