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Predictive Mineralogy

Possible unrecorded species at Gaston County, North Carolina, USA

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
MitridatiteCa2Fe3+3(PO4)3O2 路 3H2O99.97%Fairfieldite (54.32 %), Frondelite (59.68 %), Jahnsite-(CaMnMg) (52.63 %), Kastningite (90.00 %), Laueite (64.56 %), Messelite (51.02 %), Paravauxite (66.67 %), Strunzite (51.43 %)
HureauliteMn2+5(PO3OH)2(PO4)2 路 4H2O99.70%Fairfieldite (53.09 %), Frondelite (66.13 %), Jahnsite-(CaMnMg) (57.89 %), Kastningite (80.00 %), Laueite (54.43 %), Paravauxite (52.38 %)
CacoxeniteFe3+24AlO6(PO4)17(OH)12 路 75H2O98.33%Beraunite (62.09 %), Kastningite (70.00 %), Matulaite (69.23 %), Paravauxite (52.38 %)
StewartiteMn2+Fe3+2(PO4)2(OH)2 路 8H2O95.23%Kastningite (90.00 %), Paravauxite (52.38 %)
MalachiteCu2(CO3)(OH)294.97%Asbolane (51.19 %), Azurite (89.71 %)
BermaniteMn2+Mn3+2(PO4)2(OH)2 路 4H2O91.42%Kastningite (80.00 %), Paravauxite (57.14 %)
ChildreniteFe2+Al(PO4)(OH)2 路 H2O91.42%Kastningite (80.00 %), Paravauxite (57.14 %)
TorberniteCu(UO2)2(PO4)2 路 12H2O90.47%Kastningite (80.00 %), Paravauxite (52.38 %)
HessiteAg2Te79.78%Altaite (59.57 %), Nagy谩gite (50.00 %)
LeucophosphiteKFe3+2(PO4)2(OH) 路 2H2O76.31%Jahnsite-(CaMnMg) (52.63 %), Kastningite (50.00 %)
VarisciteAlPO4 路 2H2O76.19%Kastningite (50.00 %), Paravauxite (52.38 %)
MontebrasiteLiAl(PO4)(OH)75.86%Dickinsonite-(KMnNa) (51.72 %), Kastningite (50.00 %)
TitaniteCaTi(SiO4)O75.68%Bavenite (50.52 %), Hastingsite (50.85 %)
EarlshannoniteMn2+Fe3+2(PO4)2(OH)2 路 4H2O70.00%Kastningite (70.00 %)
Jahnsite-(CaMnMn){Ca}{Mn2+}{Mn2+2}{Fe3+2}(PO4)4(OH)2 路 8H2O70.00%Kastningite (70.00 %)
WavelliteAl3(PO4)2(OH,F)3 路 5H2O61.53%Matulaite (61.54 %)
BrauniteMn2+Mn3+6(SiO4)O860.86%Parsettensite (60.87 %)
BismuthiniteBi2S360.00%Bismite (60.00 %)
CryptomelaneK(Mn4+7Mn3+)O1660.00%Kastningite (60.00 %)
Jahnsite-(CaMnFe){Ca}{Mn2+}{Fe2+2}{Fe3+2}(PO4)4(OH)2 路 8H2O60.00%Kastningite (60.00 %)
MangangordoniteMn2+Al2(PO4)2(OH)2 路 8H2O60.00%Kastningite (60.00 %)
OpalSiO2 路 nH2O60.00%Kastningite (60.00 %)
RobertsiteCa2Mn3+3(PO4)3O2 路 3H2O60.00%Kastningite (60.00 %)
XanthoxeniteCa4Fe3+2(PO4)4(OH)2 路 3H2O60.00%Kastningite (60.00 %)
BismuthBi59.16%Bismite (59.17 %)
CaryopiliteMn2+3Si2O5(OH)454.34%Parsettensite (54.35 %)
TurquoiseCuAl6(PO4)4(OH)8 路 4H2O53.84%Matulaite (53.85 %)
PetziteAg3AuTe252.63%Nagy谩gite (52.63 %)
GypsumCaSO4 路 2H2O50.28%Sulphur (50.28 %)
PseudolaueiteMn2+Fe3+2(PO4)2(OH)2 路 8H2O50.00%Kastningite (50.00 %)
Rittmannite{(Mn2+,Ca)}{Mn2+}{(Fe2+,Mn2+,Mg)2}{(Al,Fe3+)2}(PO4)4(OH)2 路 8H2O50.00%Kastningite (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
34 : Complex granite pegmatites

Unique: Dickinsonite-(KMnNa), Herderite, Hydroxylherderite, Lithiophilite, Spodumene, Tantalite-(Fe), etc.
769
22 : Hydration and low-饾憞 subsurface aqueous alteration (see also #23)

Unique: Paravauxite
154
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Nagy谩gite
115
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite
105
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Parsettensite
100
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]76
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]72
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)49
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)40
26 : Hadean detrital minerals24
6 : Secondary asteroid phases17
48 : Soil leaching zone minerals16
47e : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]12
19 : Granitic intrusive rocks10
53 : Other minerals with taphonomic origins9