Predictive Mineralogy
Possible unrecorded species at Kirigo, Hizen-cho, Karatsu City, Saga Prefecture, Japan
This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.
Possible missing species | Formula | Match % | Due to recorded presence of |
---|---|---|---|
Quartz | SiO2 | 97.62% | Aragonite (53.70 %), Calcite (62.43 %), Kimuraite-(Y) (54.55 %), Lokkaite-(Y) (70.00 %) |
Pyrite | FeS2 | 80.46% | Calcite (51.16 %), Lokkaite-(Y) (60.00 %) |
Albite | Na(AlSi3O8) | 60.00% | Lokkaite-(Y) (60.00 %) |
Zircon | Zr(SiO4) | 56.00% | Lokkaite-(Y) (70.00 %) |
Fluorapatite | Ca5(PO4)3F | 50.00% | Lokkaite-(Y) (50.00 %) |
Microcline | K(AlSi3O8) | 50.00% | Lokkaite-(Y) (50.00 %) |
Xenotime-(Y) | Y(PO4) | 50.00% | Lokkaite-(Y) (50.00 %) |
Uraninite | UO2 | 48.00% | Lokkaite-(Y) (60.00 %) |
Fergusonite-(Y) | YNbO4 | 40.00% | Lokkaite-(Y) (50.00 %) |
Thorite | Th(SiO4) | 40.00% | Lokkaite-(Y) (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.