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Predictive Mineralogy

Possible unrecorded species at Oshibedani, Nishi-ku, Kobe city, Hyogo 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
QuartzSiO299.99%Beraunite (69.67 %), Cacoxenite (66.14 %), Lipscombite (70.37 %), Metavivianite (66.67 %), Mitridatite (78.81 %), Phosphosiderite (78.20 %), Rockbridgeite (71.49 %), Strunzite (81.90 %), Ushkovite (84.00 %), Vivianite (55.13 %)
PyriteFeS299.77%Beraunite (54.50 %), Cacoxenite (51.90 %), Metavivianite (69.70 %), Mitridatite (55.63 %), Phosphosiderite (50.71 %), Rockbridgeite (52.19 %), Strunzite (67.62 %)
MuscoviteKAl2(AlSi3O10)(OH)299.76%Lipscombite (57.41 %), Mitridatite (66.23 %), Phosphosiderite (56.87 %), Rockbridgeite (56.14 %), Strunzite (73.33 %), Ushkovite (68.00 %)
FluorapatiteCa5(PO4)3F97.63%Mitridatite (62.25 %), Phosphosiderite (50.71 %), Strunzite (64.76 %), Ushkovite (64.00 %)
AlbiteNa(AlSi3O8)94.25%Mitridatite (54.30 %), Strunzite (68.57 %), Ushkovite (60.00 %)
MicroclineK(AlSi3O8)92.54%Mitridatite (51.66 %), Strunzite (57.14 %), Ushkovite (64.00 %)
StrengiteFePO4 · 2H2O91.38%Beraunite (62.56 %), Phosphosiderite (53.55 %), Rockbridgeite (50.44 %)
BerylBe3Al2(Si6O18)75.26%Mitridatite (54.30 %), Strunzite (67.62 %), Ushkovite (60.00 %)
SideriteFeCO372.72%Metavivianite (72.73 %)
TriphyliteLiFe2+PO464.64%Strunzite (60.00 %), Ushkovite (52.00 %)
GypsumCaSO4 · 2H2O63.63%Metavivianite (63.64 %)
SchorlNaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)63.23%Strunzite (52.38 %), Ushkovite (56.00 %)
EosphoriteMn2+Al(PO4)(OH)2 · H2O60.00%Ushkovite (60.00 %)
Goethiteα-Fe3+O(OH)57.57%Metavivianite (57.58 %)
ZirconZr(SiO4)43.42%Strunzite (54.29 %)
SphaleriteZnS41.21%Metavivianite (51.52 %)

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
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)

Unique: Lipscombite
100
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]28
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]28
53 : Other minerals with taphonomic origins5
24 : Authigenic minerals in terrestrial sediments (see also #17)4
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]4
34 : Complex granite pegmatites3
21 : Chemically precipitated carbonate, phosphate, iron formations2
31 : Thermally altered carbonate, phosphate, and iron formations2
48 : Soil leaching zone minerals1
55 : Anthropogenic mine minerals1