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Predictive Mineralogy

Possible unrecorded species at Bauhaus, Nentershausen, Hersfeld-Rotenburg, Kassel Region, 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
QuartzSiO299.99%Annabergite (64.54 %), Baryte (60.21 %), Chalcopyrite (67.26 %), Dolomite (62.52 %), Erythrite (69.80 %), Malachite (61.21 %), Millerite (61.76 %), Nickeline (58.64 %), Nickelskutterudite (74.76 %), Rammelsbergite (69.68 %), Richelsdorfite (83.82 %)
PyriteFeS299.99%Annabergite (66.14 %), Baryte (50.79 %), Chalcopyrite (75.16 %), Dolomite (58.22 %), Erythrite (64.88 %), Malachite (52.79 %), Millerite (71.66 %), Nickeline (66.71 %), Nickelskutterudite (66.02 %), Rammelsbergite (75.09 %), Richelsdorfite (72.06 %)
CalciteCaCO399.98%Annabergite (60.16 %), Baryte (51.88 %), Dolomite (65.13 %), Erythrite (59.85 %), Millerite (53.62 %), Nickeline (56.82 %), Nickelskutterudite (65.53 %), Rammelsbergite (70.76 %), Richelsdorfite (67.65 %)
SkutteruditeCoAs380.78%Nickelskutterudite (58.74 %), Rammelsbergite (53.43 %)
GalenaPbS79.79%Annabergite (57.37 %), Chalcopyrite (51.07 %), Erythrite (53.28 %), Nickeline (55.15 %), Nickelskutterudite (59.22 %), Rammelsbergite (64.62 %), Richelsdorfite (60.29 %)
SphaleriteZnS79.68%Annabergite (52.59 %), Chalcopyrite (50.66 %), Erythrite (50.44 %), Millerite (50.48 %), Nickeline (53.48 %), Nickelskutterudite (61.65 %), Rammelsbergite (61.37 %)
AzuriteCu3(CO3)2(OH)264.70%Richelsdorfite (64.71 %)
GypsumCaSO4 · 2H2O64.70%Richelsdorfite (64.71 %)
BrochantiteCu4(SO4)(OH)655.88%Richelsdorfite (55.88 %)
CupriteCu2O55.88%Richelsdorfite (55.88 %)
OliveniteCu2(AsO4)(OH)55.88%Richelsdorfite (55.88 %)
CovelliteCuS51.47%Richelsdorfite (51.47 %)

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: Rammelsbergite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]26
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]23
37 : Layered igneous intrusions and related PGE minerals11
36 : Carbonatites, kimberlites, and related igneous rocks3
38 : Ophiolites3
53 : Other minerals with taphonomic origins3
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]3
55 : Anthropogenic mine minerals1
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]1
50 : Coal and/or oil shale minerals0