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Predictive Mineralogy

Possible unrecorded species at Steinerleinbach Quarry, Röhrnbach, Freyung-Grafenau District, Lower Bavaria, Bavaria, 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
MagnetiteFe2+Fe3+2O499.75%Actinolite (53.38 %), Andradite (57.68 %), Augite (53.49 %), Caysichite-(Y) (50.00 %), Ferro-hornblende (64.86 %), Ilmenite (57.89 %), Parisite-(Ce) (63.70 %)
ArsenopyriteFeAsS98.73%Cosalite (55.33 %), Galenobismutite (55.76 %), Gersdorffite (50.38 %), Joséite-B (73.00 %), Lillianite (52.05 %)
DiopsideCaMgSi2O688.89%Grossular (52.27 %), Vesuvianite (52.97 %), Wollastonite (50.54 %)
GoldAu79.68%Galenobismutite (53.92 %), Joséite-B (72.00 %), Lillianite (54.11 %), Tellurium (76.37 %), Tetradymite (71.62 %)
ChalcociteCu2S79.29%Covellite (50.30 %), Villamanínite (58.33 %)
AzuriteCu3(CO3)2(OH)277.46%Cuprite (51.54 %), Langite (53.49 %)
TripliteMn2+2(PO4)F60.78%Zwieselite (60.78 %)
ThoriteTh(SiO4)60.00%Caysichite-(Y) (60.00 %)
Xenotime-(Y)Y(PO4)60.00%Caysichite-(Y) (60.00 %)
Bastnäsite-(Ce)Ce(CO3)F58.90%Parisite-(Ce) (58.90 %)
CopiapiteFe2+Fe3+4(SO4)6(OH)2 · 20H2O58.86%Römerite (58.87 %)
BorniteCu5FeS458.33%Villamanínite (58.33 %)
SmithsoniteZnCO355.58%Hemimorphite (55.59 %)
CopperCu53.09%Pumpellyite-(Mg) (53.10 %)
HessiteAg2Te51.47%Tellurium (51.48 %)
SilverAg50.31%Acanthite (50.32 %)
PreisingeriteBi3(AsO4)2O(OH)50.00%Petitjeanite (50.00 %)
DigeniteCu9S550.00%Villamanínite (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
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite, Stolzite, Wulfenite
297
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Cosalite, Eulytine
265
34 : Complex granite pegmatites

Unique: Bazzite, Zwieselite
231
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Pumpellyite-(Mg)
101
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Villamanínite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]45
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)32
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]30
31 : Thermally altered carbonate, phosphate, and iron formations26
26 : Hadean detrital minerals22
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]21
36 : Carbonatites, kimberlites, and related igneous rocks17
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)16
49 : Oxic cellular biomineralization (see also #44)15
37 : Layered igneous intrusions and related PGE minerals13