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Predictive Mineralogy

Possible unrecorded species at Philippshoffnung Mine, Siegen, Siegen-Wittgenstein, Arnsberg, North Rhine-Westphalia, 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%Arsenopyrite (79.40 %), Asbolane (54.76 %), Chalcopyrite (75.16 %), Cobaltite (78.87 %), Erythrite (64.88 %), Gersdorffite (82.91 %), Siderite (66.11 %), Skutterudite (62.40 %)
CalciteCaCO399.75%Aragonite (71.64 %), Asbolane (50.00 %), Cobaltite (51.81 %), Erythrite (59.85 %), Gersdorffite (53.89 %), Siderite (52.18 %), Skutterudite (59.07 %)
GalenaPbS79.44%Arsenopyrite (53.61 %), Chalcopyrite (51.07 %), Cobaltite (57.74 %), Erythrite (53.28 %), Gersdorffite (68.13 %), Skutterudite (51.58 %)
PyrrhotiteFe1-xS79.10%Cobaltite (57.03 %), Gersdorffite (51.37 %)
SphaleriteZnS78.82%Arsenopyrite (55.02 %), Chalcopyrite (50.66 %), Cobaltite (60.74 %), Erythrite (50.44 %), Gersdorffite (65.94 %)
MalachiteCu2(CO3)(OH)276.12%Asbolane (51.19 %), Erythrite (51.09 %)
SilverAg40.73%Skutterudite (50.92 %)

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])50
37 : Layered igneous intrusions and related PGE minerals44
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]24
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]21
36 : Carbonatites, kimberlites, and related igneous rocks7
38 : Ophiolites7
42 : Sea-floor Mn nodules3
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]3
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)3
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)1