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 species | Formula | Match % | Due to recorded presence of |
---|---|---|---|
Quartz | SiO2 | 99.99% | 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 %) |
Pyrite | FeS2 | 99.77% | Beraunite (54.50 %), Cacoxenite (51.90 %), Metavivianite (69.70 %), Mitridatite (55.63 %), Phosphosiderite (50.71 %), Rockbridgeite (52.19 %), Strunzite (67.62 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 99.76% | Lipscombite (57.41 %), Mitridatite (66.23 %), Phosphosiderite (56.87 %), Rockbridgeite (56.14 %), Strunzite (73.33 %), Ushkovite (68.00 %) |
Fluorapatite | Ca5(PO4)3F | 97.63% | Mitridatite (62.25 %), Phosphosiderite (50.71 %), Strunzite (64.76 %), Ushkovite (64.00 %) |
Albite | Na(AlSi3O8) | 94.25% | Mitridatite (54.30 %), Strunzite (68.57 %), Ushkovite (60.00 %) |
Microcline | K(AlSi3O8) | 92.54% | Mitridatite (51.66 %), Strunzite (57.14 %), Ushkovite (64.00 %) |
Strengite | FePO4 · 2H2O | 91.38% | Beraunite (62.56 %), Phosphosiderite (53.55 %), Rockbridgeite (50.44 %) |
Beryl | Be3Al2(Si6O18) | 75.26% | Mitridatite (54.30 %), Strunzite (67.62 %), Ushkovite (60.00 %) |
Siderite | FeCO3 | 72.72% | Metavivianite (72.73 %) |
Triphylite | LiFe2+PO4 | 64.64% | Strunzite (60.00 %), Ushkovite (52.00 %) |
Gypsum | CaSO4 · 2H2O | 63.63% | Metavivianite (63.64 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 63.23% | Strunzite (52.38 %), Ushkovite (56.00 %) |
Eosphorite | Mn2+Al(PO4)(OH)2 · H2O | 60.00% | Ushkovite (60.00 %) |
Goethite | α-Fe3+O(OH) | 57.57% | Metavivianite (57.58 %) |
Zircon | Zr(SiO4) | 43.42% | Strunzite (54.29 %) |
Sphalerite | ZnS | 41.21% | 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.