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Predictive Mineralogy

Possible unrecorded species at North Bohemian Uranium District, Liberec 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
MalachiteCu2(CO3)(OH)299.87%Anglesite (50.35 %), Arsenogoyazite (60.87 %), Asbolane (51.19 %), Chalcanthite (62.86 %), Chalcocite (56.20 %), Covellite (54.66 %), Duranusite (50.00 %), Philipsbornite (64.52 %)
AlbiteNa(AlSi3O8)99.72%Allanite-(Ce) (52.28 %), Cheralite (69.32 %), Chernovite-(Y) (52.63 %), Monazite-(Ce) (51.78 %), Rhabdophane-(Ce) (54.22 %), Synchysite-(Ce) (60.21 %), Synchysite-(Y) (54.84 %)
Goethite伪-Fe3+O(OH)98.42%Arsenogoyazite (60.87 %), Churchite-(Y) (50.00 %), Coronadite (52.03 %), Duranusite (58.33 %), Philipsbornite (59.68 %)
BorniteCu5FeS496.05%Carrollite (70.95 %), Stromeyerite (51.92 %), Wittichenite (71.78 %)
IlmeniteFe2+TiO390.98%Armalcolite (58.70 %), Baddeleyite (56.36 %), Pseudorutile (50.00 %)
OrpimentAs2S386.17%Duranusite (66.67 %), Realgar (58.53 %)
MagnetiteFe2+Fe3+2O484.30%Baddeleyite (60.00 %), Hercynite (60.77 %)
SulphurS882.47%Mohrite (60.00 %), Tschermigite (56.18 %)
PyrargyriteAg3SbS381.42%Polybasite (55.84 %), Stephanite (57.94 %)
MilleriteNiS78.47%Siegenite (51.19 %), Vaesite (55.91 %)
AzuriteCu3(CO3)2(OH)278.40%Arsenogoyazite (52.17 %), Philipsbornite (54.84 %)
HaliteNaCl78.14%Mohrite (50.00 %), Th茅nardite (56.29 %)
TorberniteCu(UO2)2(PO4)2 路 12H2O77.14%Tr枚gerite (52.17 %), Uranopilite (52.21 %)
TitaniteCaTi(SiO4)O76.26%Allanite-(Ce) (52.52 %), Synchysite-(Ce) (50.00 %)
ArsenicAs66.66%Duranusite (66.67 %)
MimetitePb5(AsO4)3Cl66.12%Philipsbornite (66.13 %)
Mascagnite(NH4)2SO465.00%Mohrite (65.00 %)
BournonitePbCuSbS359.75%Seligmannite (59.76 %)
ArsenoliteAs2O358.33%Duranusite (58.33 %)
ScoroditeFe3+AsO4 路 2H2O58.06%Philipsbornite (58.06 %)
ZeuneriteCu(UO2)2(AsO4)2 路 12H2O56.52%Tr枚gerite (56.52 %)
BismuthBi55.88%Waylandite (55.88 %)
ThoriteTh(SiO4)55.76%Brockite (55.77 %)
PyromorphitePb5(PO4)3Cl55.44%Plumbogummite (55.45 %)
ChlorargyriteAgCl53.84%Bromargyrite (53.85 %)
Bismutite(BiO)2CO352.94%Waylandite (52.94 %)
AluniteKAl3(SO4)2(OH)652.77%Woodhouseite (52.78 %)
ConichalciteCaCu(AsO4)(OH)52.17%Arsenogoyazite (52.17 %)
BeudantitePbFe3(AsO4)(SO4)(OH)651.61%Philipsbornite (51.61 %)
UranophaneCa(UO2)2(SiO3OH)2 路 5H2O51.32%Uranopilite (51.33 %)
HexahydriteMgSO4 路 6H2O50.00%Mohrite (50.00 %)
SalammoniacNH4Cl50.00%Mohrite (50.00 %)
Bastn盲site-(Ce)Ce(CO3)F50.00%Synchysite-(Nd) (50.00 %)
AegirineNaFe3+Si2O650.00%Calkinsite-(Ce) (50.00 %)
Burbankite(Na,Ca)3(Sr,Ba,Ce)3(CO3)550.00%Calkinsite-(Ce) (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: Clausthalite, Duranusite, Dyscrasite, Gudmundite, Langisite, Naumannite, etc.
1,479
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Cattierite, Jordisite, Siegenite, Vaesite
411
34 : Complex granite pegmatites

Unique: Brockite, Rhabdophane-(Nd)
253
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Pseudorutile, Wulfenite
210
47g : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Bromargyrite
100
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]84
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]82
37 : Layered igneous intrusions and related PGE minerals52
35 : Ultra-alkali and agpaitic igneous rocks42
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)35
26 : Hadean detrital minerals34
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]34
36 : Carbonatites, kimberlites, and related igneous rocks30
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]24
47b : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]22