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Predictive Mineralogy

Possible unrecorded species at Krufter Ofen, Kruft, Pellenz, Mayen-Koblenz, Rhineland-Palatinate, 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
SphaleriteZnS99.98%Bustamite (53.78 %), Chalcopyrite (50.66 %), Devilline (62.38 %), Digenite (61.34 %), Fergusonite-(Ce) (52.38 %), Hydrozincite (77.75 %), Marcasite (65.85 %), Melanterite (50.38 %), Pyrrhotite (55.40 %), Rhabdophane-(Ce) (50.60 %)
AegirineNaFe3+Si2O699.84%Cancrinite (57.33 %), Fergusonite-(Ce) (57.14 %), Fluorcalciopyrochlore (68.97 %), Hiortdahlite (68.97 %), Låvenite (78.65 %), Wöhlerite (58.33 %)
ThoriteTh(SiO4)98.17%Fergusonite-(Ce) (61.90 %), Hiortdahlite (55.17 %), Huttonite (77.50 %), Nioboaeschynite-(Ce) (52.38 %)
SodaliteNa4(Si3Al3)O12Cl96.51%Cancrinite (57.33 %), Götzenite (52.94 %), Hiortdahlite (51.72 %), Låvenite (64.04 %)
MicroclineK(AlSi3O8)96.14%Columbite-(Mn) (62.20 %), Fergusonite-(Y) (53.52 %), Fersmite (53.98 %), Wöhlerite (52.27 %)
ChalcociteCu2S95.87%Anilite (67.86 %), Digenite (65.40 %), Djurleite (62.90 %)
BorniteCu5FeS495.83%Anilite (63.39 %), Digenite (68.36 %), Djurleite (64.06 %)
CovelliteCuS95.04%Anilite (59.82 %), Digenite (72.00 %), Djurleite (55.94 %)
AnalcimeNa(AlSi2O6) · H2O82.53%Låvenite (57.30 %), Wöhlerite (59.09 %)
HaliteNaCl81.53%Sylvite (81.54 %)
GalenaPbS79.90%Anilite (50.00 %), Chalcopyrite (51.07 %), Devilline (66.36 %), Digenite (59.98 %), Djurleite (51.01 %), Hydrozincite (82.83 %), Marcasite (58.73 %)
BrochantiteCu4(SO4)(OH)671.26%Devilline (71.26 %)
CerussitePbCO367.45%Devilline (52.10 %), Hydrozincite (67.25 %)
Chevkinite-(Ce)Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)266.66%Nioboaeschynite-(Ce) (66.67 %)
SmithsoniteZnCO362.08%Hydrozincite (62.08 %)
NatroliteNa2Al2Si3O10 · 2H2O61.36%Wöhlerite (61.36 %)
EudialyteNa15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)257.30%Låvenite (57.30 %)
AnorthiteCa(Al2Si2O8)57.14%Davyne (57.14 %)
BerylBe3Al2(Si6O18)56.66%Columbite-(Mn) (70.83 %)
CupriteCu2O53.50%Devilline (53.50 %)
HemimorphiteZn4Si2O7(OH)2 · H2O52.66%Hydrozincite (52.67 %)
HausmanniteMn2+Mn3+2O452.52%Jacobsite (52.53 %)
KaoliniteAl2(Si2O5)(OH)451.68%Alunite (51.69 %)

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
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Götzenite, Hiortdahlite, Låvenite
287
34 : Complex granite pegmatites104
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Halloysite
100
26 : Hadean detrital minerals76
36 : Carbonatites, kimberlites, and related igneous rocks29
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)25
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]19
31 : Thermally altered carbonate, phosphate, and iron formations17
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits14
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)14
9 : Lava/xenolith minerals (hornfels, sanidinite facies)11
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])11