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Predictive Mineralogy

Possible unrecorded species at Ústí nad Labem Region, Czech Republic

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
LarniteCa2SiO497.74%Barioferrite (71.43 %), Bredigite (84.21 %), Srebrodolskite (50.00 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O95.86%Natrouranospinite (50.00 %), Phosphuranylite (64.29 %), Schoepite (52.21 %), Torbernite (51.52 %)
KotulskitePd(Te,Bi)2-x (x ≈ 0.4)91.00%Merenskyite (53.06 %), Michenerite (55.19 %), Moncheite (57.22 %)
AdamiteZn2(AsO4)(OH)89.42%Mawbyite (54.17 %), Thometzekite (53.85 %), Zincolivenite (50.00 %)
BournonitePbCuSbS382.41%Fülöppite (54.55 %), Semseyite (61.32 %)
DjurleiteCu31S1680.24%Anilite (56.25 %), Roxbyite (54.84 %)
GartrellitePbCuFe3+(AsO4)2(OH) · H2O78.84%Mawbyite (54.17 %), Thometzekite (53.85 %)
LeadhillitePb4(CO3)2(SO4)(OH)278.32%Susannite (53.04 %), Thometzekite (53.85 %)
SpionkopiteCu39S2873.49%Yarrowite (73.49 %)
CarnalliteKMgCl3 · 6H2O70.14%Kainite (70.15 %)
ZinkenitePb9Sb22S4269.69%Fülöppite (69.70 %)
UranospiniteCa(UO2)2(AsO4)2 · 10H2O68.75%Natrouranospinite (68.75 %)
SpurriteCa5(SiO4)2(CO3)68.42%Bredigite (68.42 %)
CobaltiteCoAsS66.66%Vavřínite (66.67 %)
MawsoniteCu6Fe2SnS863.54%Stannoidite (63.54 %)
BoulangeritePb5Sb4S1160.37%Semseyite (60.38 %)
CaledonitePb5Cu2(SO4)3(CO3)(OH)658.26%Susannite (58.26 %)
AtacamiteCu2(OH)3Cl57.50%Nantokite (57.50 %)
TyroliteCa2Cu9(AsO4)4(CO3)(OH)8 · 11H2O57.39%Strashimirite (57.39 %)
FluorellestaditeCa5(SiO4)1.5(SO4)1.5F57.14%Barioferrite (57.14 %)
ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)56.25%Trilithionite (56.25 %)
KtenasiteZnCu4(SO4)2(OH)6 · 6H2O54.54%Gordaite (54.55 %)
MetavoltineK2Na6Fe2+Fe3+6O2(SO4)12 · 18H2O53.84%Kremersite (53.85 %)
SeleniumSe53.84%Kremersite (53.85 %)
VoltaiteK2Fe2+5Fe3+3Al(SO4)12 · 18H2O53.84%Kremersite (53.85 %)
ChalcanthiteCuSO4 · 5H2O53.84%Thometzekite (53.85 %)
HidalgoitePbAl3(AsO4)(SO4)(OH)653.84%Thometzekite (53.85 %)
Lepidocrociteγ-Fe3+O(OH)53.84%Thometzekite (53.85 %)
Pitticite(Fe, AsO4, H2O) (?)53.84%Thometzekite (53.85 %)
TyuyamuniteCa(UO2)2(VO4)2 · 5-8H2O53.33%Metatyuyamunite (53.33 %)
PericlaseMgO52.94%Srebrodolskite (52.94 %)
MerwiniteCa3Mg(SiO4)252.63%Bredigite (52.63 %)
HydrocerussitePb3(CO3)2(OH)251.30%Susannite (51.30 %)
TetradymiteBi2Te2S51.06%Kawazulite (51.06 %)
SylviteKCl50.74%Kainite (50.75 %)
RosenbuschiteNa6Ca6Zr3Ti(Si2O7)4O2F650.00%Hainite-(Y) (50.00 %)
ParauranophaneCa(UO2)2(SiO3OH)2 · 5H2O50.00%Natrouranospinite (50.00 %)
GuériniteCa6(HAsO4)3(AsO4)2 · 10.5H2O50.00%Weilite (50.00 %)
HaidingeriteCaHAsO4 · H2O50.00%Weilite (50.00 %)
SainfelditeCa5(AsO4)2(AsO3OH)2 · 4H2O50.00%Weilite (50.00 %)
NatrojarositeNaFe3(SO4)2(OH)650.00%Gordaite (50.00 %)
SpessartineMn2+3Al2(SiO4)350.00%Trilithionite (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: Aikinite, Argentopyrite, Arsenic, Bohdanowiczite, Clausthalite, Emplectite, etc.
3,247
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Ferrimolybdite, Halloysite
573
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite, Koechlinite, Russellite, Wulfenite
407
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Jordisite, Kësterite, Polydymite, Roxbyite
368
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]329
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)

Unique: Cowlesite, Garronite-Ca, Gismondine Subgroup
315
34 : Complex granite pegmatites

Unique: Polylithionite, Trilithionite
295
10 : Basalt-hosted zeolite minerals

Unique: Lévyne-Ca, Offretite, Tschernichite
280
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Hörnesite, Tobermorite
212
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
193
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Hainite-(Y)
145
36 : Carbonatites, kimberlites, and related igneous rocks

Unique: Bastnäsite-(La)
129
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)110
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
100
37 : Layered igneous intrusions and related PGE minerals76
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]70
26 : Hadean detrital minerals69
50 : Coal and/or oil shale minerals69
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)68
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]51
54 : Coal and other mine fire minerals (see also #51 and #56)50
53 : Other minerals with taphonomic origins49