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Predictive Mineralogy

Possible unrecorded species at Fujii mine, Wakasa-cho, Mikatakaminaka District, Fukui Prefecture, Japan

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
CalciteCaCO399.99%Allanite-(La) (58.62 %), Bustamite (65.55 %), Caryopilite (70.33 %), Goldmanite (66.67 %), Hausmannite (51.00 %), Jacobsite (52.02 %), Kellyite (56.25 %), Manganosite (54.88 %), Nickeline (56.82 %), Pyrochroite (71.88 %), Rhodochrosite (50.69 %), Sussexite (63.33 %)
PyriteFeS299.98%Allanite-(La) (55.17 %), Bustamite (58.82 %), Goldmanite (75.00 %), Kellyite (50.00 %), Molybdenite (68.29 %), Nickeline (66.71 %), Pyrochroite (50.00 %), Rhodochrosite (56.95 %), Sussexite (70.00 %)
AlleghanyiteMn2+5(SiO4)2(OH)290.62%Kellyite (50.00 %), Sonolite (57.14 %), Wiserite (56.25 %)
MuscoviteKAl2(AlSi3O10)(OH)278.51%Goldmanite (52.78 %), Spessartine (54.51 %)
ChalcopyriteCuFeS278.11%Bustamite (52.94 %), Goldmanite (52.78 %), Molybdenite (60.83 %), Nickeline (72.98 %)
BaryteBaSO477.75%Manganosite (58.54 %), Pyrochroite (68.75 %), Sussexite (56.67 %), Wiserite (50.00 %)
MagnetiteFe2+Fe3+2O477.58%Allanite-(La) (55.17 %), Sussexite (50.00 %)
HematiteFe2O376.61%Allanite-(La) (51.72 %), Pyrochroite (51.56 %)
SphaleriteZnS72.54%Bustamite (53.78 %), Nickeline (53.48 %), Sussexite (56.67 %)
GalenaPbS62.06%Nickeline (55.15 %), Sussexite (50.00 %)
PyrophaniteMn2+TiO360.76%Galaxite (51.92 %), Kellyite (50.00 %)
AlbiteNa(AlSi3O8)58.62%Allanite-(La) (58.62 %)
PyrrhotiteFe1-xS50.00%Goldmanite (50.00 %)
ZirconZr(SiO4)49.65%Allanite-(La) (62.07 %)
TitaniteCaTi(SiO4)O46.89%Allanite-(La) (58.62 %)
Allanite-(Ce)(CaCe)(AlAlFe2+)O[Si2O7][SiO4](OH)41.37%Allanite-(La) (51.72 %)

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
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hausmannite, Momoiite
209
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Sussexite
100
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)24
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)13
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])13
35 : Ultra-alkali and agpaitic igneous rocks13
37 : Layered igneous intrusions and related PGE minerals10
31 : Thermally altered carbonate, phosphate, and iron formations9
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]4
19 : Granitic intrusive rocks3
6 : Secondary asteroid phases3
21 : Chemically precipitated carbonate, phosphate, iron formations3