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Predictive Mineralogy

Possible unrecorded species at Dob拧in谩 mining district, Dob拧in谩, Ro啪艌ava District, Ko拧ice Region, Slovakia

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
SilverAg99.88%Gu茅rinite (72.97 %), Pararammelsbergite (50.85 %), Pharmacolite (54.31 %), Phaunouxite (63.16 %), Rauenthalite (73.33 %), Safflorite (59.63 %), Skutterudite (50.92 %)
MicroclineK(AlSi3O8)99.49%Columbite-(Mn) (62.20 %), Elbaite (53.90 %), Fersmite (53.98 %), Fluor-elbaite (54.29 %), Hydroxycalciomicrolite (64.29 %), Hydroxycalciopyrochlore (61.11 %)
ChalcociteCu2S96.98%Covellite (50.30 %), Digenite (65.40 %), Tennantite-(Cu) (60.00 %), Wittichenite (56.16 %)
CupriteCu2O90.80%Botallackite (50.88 %), Devilline (53.50 %), Langite (59.73 %)
FluoriteCaF289.66%Gu茅rinite (54.05 %), Huttonite (55.00 %), Hydroxycalciopyrochlore (50.00 %)
SainfelditeCa5(AsO4)2(AsO3OH)2 路 4H2O81.62%Gu茅rinite (54.05 %), Rauenthalite (60.00 %)
BerylBe3Al2(Si6O18)79.62%Columbite-(Mn) (70.83 %), Elbaite (60.85 %), Fluor-elbaite (71.43 %), Hydroxycalciomicrolite (85.71 %)
ArsenicAs79.47%Phaunouxite (52.63 %), Rauenthalite (56.67 %)
GoldAu78.96%Bohdanowiczite (57.14 %), Clausthalite (51.11 %), Naumannite (66.53 %), Tennantite-(Cu) (60.00 %), Wittichenite (53.97 %)
CerussitePbCO377.93%Devilline (52.10 %), Langite (53.94 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 路 nH2O, x < 166.66%Tangdanite (66.67 %)
OliveniteCu2(AsO4)(OH)66.66%Tangdanite (66.67 %)
RhodochrositeMnCO361.61%Jacobsite (61.62 %)
TyroliteCa2Cu9(AsO4)4(CO3)(OH)8 路 11H2O60.00%Tangdanite (60.00 %)
BismuthiniteBi2S357.14%Ferroskutterudite (57.14 %)
ConnelliteCu19(SO4)(OH)32Cl4 路 3H2O54.38%Botallackite (54.39 %)
TitaniteCaTi(SiO4)O53.98%Fersmite (53.98 %)
AcanthiteAg2S53.33%Rauenthalite (53.33 %)
ChalcophylliteCu18Al2(AsO4)4(SO4)3(OH)24 路 36H2O53.33%Tangdanite (53.33 %)
HausmanniteMn2+Mn3+2O452.52%Jacobsite (52.53 %)
RhodoniteCaMn3Mn[Si5O15]50.00%Jacobsite (50.00 %)
Tapiolite-(Fe)Fe2+Ta2O650.00%Hydroxycalciomicrolite (50.00 %)
Tantalite-(Mn)Mn2+Ta2O650.00%Hydroxycalciomicrolite (50.00 %)
Cordierite(Mg,Fe)2Al3(AlSi5O18)50.00%Prismatine (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: Bohdanowiczite, Clausthalite, Enargite, Freibergite Subgroup, Krutovite, Naumannite, etc.
1,115
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Kornerupine, Prismatine
215
34 : Complex granite pegmatites

Unique: Hydroxycalciomicrolite
170
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]109
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Spherocobaltite
104
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: H枚rnesite
102
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Luzonite
100
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]80
37 : Layered igneous intrusions and related PGE minerals49
26 : Hadean detrital minerals48
35 : Ultra-alkali and agpaitic igneous rocks28
36 : Carbonatites, kimberlites, and related igneous rocks27
38 : Ophiolites25
55 : Anthropogenic mine minerals20
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits18
47b : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]12