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Predictive Mineralogy

Possible unrecorded species at Wingertsberg Quarry, Nieder-Ramstadt, Mühltal, Darmstadt-Dieburg, 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
ArsenopyriteFeAsS87.59%Gersdorffite (50.38 %), Krutovite (75.00 %)
DolomiteCaMg(CO3)284.52%Krutovite (68.75 %), Nickelskutterudite (50.49 %)
SkutteruditeCoAs382.78%Nickelskutterudite (58.74 %), Safflorite (58.29 %)
GoldAu66.90%Clausthalite (51.11 %), Naumannite (66.53 %)
UmangiteCu3Se266.12%Eucairite (66.13 %)
CobaltiteCoAsS62.50%Krutovite (62.50 %)
KlockmanniteCuSe59.67%Eucairite (59.68 %)
Pentlandite(NixFey)Σ9S858.42%Maucherite (58.42 %)
LöllingiteFeAs256.25%Krutovite (56.25 %)
RammelsbergiteNiAs256.25%Krutovite (56.25 %)
BerzelianiteCu2-xSe (x ≈ 0.12)54.83%Eucairite (54.84 %)
DigeniteCu9S553.45%Idaite (53.46 %)
MarcasiteFeS250.00%Krutovite (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: Betekhtinite, Clausthalite, Eucairite, Krutovite, Maucherite, Naumannite, etc.
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]4
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]4
37 : Layered igneous intrusions and related PGE minerals2
53 : Other minerals with taphonomic origins1
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)1
6 : Secondary asteroid phases1
49 : Oxic cellular biomineralization (see also #44)1
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]1
36 : Carbonatites, kimberlites, and related igneous rocks0
38 : Ophiolites0