Predictive Mineralogy
Possible unrecorded species at Pegmatite vein Old艡ich, Doln铆 Bory, Bory, 沤膹谩r nad S谩zavou District, Vyso膷ina Region, Czech Republic
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 |
---|---|---|---|
Fluorapatite | Ca5(PO4)3F | 99.96% | Earlshannonite (73.33 %), Fairfieldite (80.25 %), Laueite (68.35 %), Scorzalite (56.34 %), Strunzite (64.76 %), Whitmoreite (71.43 %), Zwieselite (58.82 %) |
Galena | PbS | 99.92% | Bismuth (51.78 %), Bismuthinite (57.89 %), Bournonite (85.29 %), Chalcopyrite (51.07 %), L枚llingite (53.52 %), Parasymplesite (55.32 %), Sphalerite (74.68 %) |
Calcite | CaCO3 | 99.89% | Bournonite (55.32 %), Dolomite (65.13 %), L枚llingite (51.02 %), Montmorillonite (52.16 %), Nontronite (51.54 %), Palygorskite (62.61 %), Parasymplesite (65.96 %), Siderite (52.18 %) |
Arsenopyrite | FeAsS | 99.72% | Bournonite (55.79 %), Earlshannonite (80.00 %), Laueite (51.90 %), L枚llingite (65.68 %), Parasymplesite (55.32 %), Whitmoreite (57.14 %) |
Strengite | FePO4 路 2H2O | 99.41% | Beraunite (62.56 %), Earlshannonite (73.33 %), Laueite (50.63 %), Paulkerrite (50.00 %), Rockbridgeite (50.44 %), Whitmoreite (52.38 %) |
Phosphosiderite | FePO4 路 2H2O | 99.31% | Earlshannonite (73.33 %), Laueite (70.89 %), Paulkerrite (50.00 %), Strunzite (59.05 %), Whitmoreite (57.14 %) |
Mitridatite | Ca2Fe3+3(PO4)3O2 路 3H2O | 98.81% | Earlshannonite (66.67 %), Fairfieldite (54.32 %), Laueite (64.56 %), Strunzite (51.43 %), Whitmoreite (54.76 %) |
Hureaulite | Mn2+5(PO3OH)2(PO4)2 路 4H2O | 95.72% | Earlshannonite (80.00 %), Fairfieldite (53.09 %), Laueite (54.43 %) |
Heterosite | (Fe3+,Mn3+)PO4 | 93.58% | Alluaudite (55.66 %), Laueite (62.03 %), Whitmoreite (61.90 %) |
Beryl | Be3Al2(Si6O18) | 79.99% | Alluaudite (66.04 %), Beusite (50.00 %), Cookeite (60.68 %), Earlshannonite (73.33 %), Fairfieldite (77.78 %), Laueite (74.68 %), Strunzite (67.62 %), Triphylite (71.97 %), Triplite (65.10 %), Whitmoreite (54.76 %), Zwieselite (56.86 %) |
Eosphorite | Mn2+Al(PO4)(OH)2 路 H2O | 79.83% | Earlshannonite (53.33 %), Fairfieldite (56.79 %) |
Graftonite | Fe2+Fe2+2(PO4)2 | 71.83% | Sarcopside (71.83 %) |
Frondelite | Mn2+Fe3+4(PO4)3(OH)5 | 66.66% | Earlshannonite (66.67 %) |
Stewartite | Mn2+Fe3+2(PO4)2(OH)2 路 8H2O | 66.66% | Earlshannonite (66.67 %) |
Cassiterite | SnO2 | 62.02% | Earlshannonite (53.33 %), Fairfieldite (51.85 %) |
Scorodite | Fe3+AsO4 路 2H2O | 56.73% | Parasymplesite (56.74 %) |
Bermanite | Mn2+Mn3+2(PO4)2(OH)2 路 4H2O | 53.33% | Earlshannonite (53.33 %) |
Childrenite | Fe2+Al(PO4)(OH)2 路 H2O | 53.33% | Earlshannonite (53.33 %) |
Jahnsite-(CaMnFe) | {Ca}{Mn2+}{Fe2+2}{Fe3+2}(PO4)4(OH)2 路 8H2O | 53.33% | Earlshannonite (53.33 %) |
Jahnsite-(CaMnMn) | {Ca}{Mn2+}{Mn2+2}{Fe3+2}(PO4)4(OH)2 路 8H2O | 53.33% | Earlshannonite (53.33 %) |
Leucophosphite | KFe3+2(PO4)2(OH) 路 2H2O | 53.33% | Earlshannonite (53.33 %) |
Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) | 50.00% | Cookeite (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.