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Predictive Mineralogy

Possible unrecorded species at Masaki (Mazaki), Kawasaki, Tagawa-gun, Fukuoka 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
QuartzSiO299.93%Allanite-(Ce) (73.19 %), Microcline (81.52 %), Synchysite-(Ce) (81.69 %), Torbernite (60.62 %), Uraninite (52.94 %), Zircon (64.02 %)
AlbiteNa(AlSi3O8)91.66%Allanite-(Ce) (52.28 %), Microcline (56.11 %), Synchysite-(Ce) (60.21 %)
PyriteFeS284.09%Synchysite-(Ce) (67.25 %), Uraninite (51.44 %)
CalciteCaCO372.53%Synchysite-(Ce) (72.54 %)
MuscoviteKAl2(AlSi3O10)(OH)261.50%Microcline (61.50 %)
TitaniteCaTi(SiO4)O61.00%Allanite-(Ce) (52.52 %), Synchysite-(Ce) (50.00 %)
FluoriteCaF260.91%Synchysite-(Ce) (60.92 %)
HematiteFe2O351.76%Synchysite-(Ce) (51.76 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O51.51%Torbernite (51.52 %)
AnataseTiO241.12%Synchysite-(Ce) (51.41 %)

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
35 : Ultra-alkali and agpaitic igneous rocks50
34 : Complex granite pegmatites50
36 : Carbonatites, kimberlites, and related igneous rocks39
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]36
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]36
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]36
26 : Hadean detrital minerals14
19 : Granitic intrusive rocks11
24 : Authigenic minerals in terrestrial sediments (see also #17)8
8 : Mafic igneous rocks3