Predictive Mineralogy
Possible unrecorded species at Binn, Goms, Valais, Switzerland
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 |
---|---|---|---|
Stibnite | Sb2S3 | 99.48% | Aktashite (70.83 %), Lor谩ndite (52.63 %), Parapierrotite (83.33 %), Routhierite (77.78 %) |
Cassiterite | SnO2 | 96.25% | Canfieldite (58.10 %), 膶ern媒ite (80.00 %), K毛sterite (55.32 %) |
Stannite | Cu2FeSnS4 | 95.31% | Canfieldite (58.10 %), 膶ern媒ite (70.00 %), K毛sterite (62.77 %) |
Braunite | Mn2+Mn3+6(SiO4)O8 | 95.05% | Gasparite-(La) (87.50 %), Tilasite (60.47 %) |
Analcime | Na(AlSi2O6) 路 H2O | 91.08% | Mesolite (52.00 %), Natrolite (56.38 %), Thomsonite-Ca (57.41 %) |
Aegirine | NaFe3+Si2O6 | 84.55% | Gasparite-(La) (62.50 %), Thalcusite (58.82 %) |
Zinkenite | Pb9Sb22S42 | 83.33% | Parapierrotite (50.00 %), Routhierite (66.67 %) |
L枚llingite | FeAs2 | 81.63% | Arsenolamprite (57.14 %), Dervillite (57.14 %) |
Hammarite | Pb2Cu2Bi4S9 | 81.25% | Paarite (50.00 %), Salzburgite (62.50 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 81.14% | Rosasite (59.34 %), Theisite (53.62 %) |
Bismuth | Bi | 80.20% | 膶ern媒ite (60.00 %), Krupkaite (50.52 %) |
Pyromorphite | Pb5(PO4)3Cl | 80.03% | Dervillite (57.14 %), Leadhillite (53.42 %) |
Autunite | Ca(UO2)2(PO4)2 路 10-12H2O | 79.17% | Meta-autunite (57.04 %), Torbernite (51.52 %) |
Chlorargyrite | AgCl | 71.42% | Dervillite (71.43 %) |
Erythrite | Co3(AsO4)2 路 8H2O | 71.39% | H枚rnesite (52.00 %), Pharmacolite (55.17 %), Picropharmacolite (50.00 %) |
Mascagnite | (NH4)2SO4 | 65.00% | Mohrite (65.00 %) |
Hausmannite | Mn2+Mn3+2O4 | 62.50% | Gasparite-(La) (62.50 %) |
Rhodochrosite | MnCO3 | 62.50% | Gasparite-(La) (62.50 %) |
Rhodonite | CaMn3Mn[Si5O15] | 62.50% | Gasparite-(La) (62.50 %) |
Melanterite | Fe2+(H2O)6SO4 路 H2O | 60.00% | Ferrohexahydrite (60.00 %) |
Tschermigite | (NH4)Al(SO4)2 路 12H2O | 60.00% | Mohrite (60.00 %) |
Bastn盲site-(Ce) | Ce(CO3)F | 58.90% | Parisite-(Ce) (58.90 %) |
Cornwallite | Cu5(AsO4)2(OH)4 | 57.69% | Cornubite (57.69 %) |
Argentopyrite | AgFe2S3 | 57.14% | Dervillite (57.14 %) |
Dyscrasite | Ag3Sb | 57.14% | Dervillite (57.14 %) |
Fluckite | CaMn2+(AsO3OH)2 路 2H2O | 57.14% | Dervillite (57.14 %) |
Gu茅rinite | Ca6(HAsO4)3(AsO4)2 路 10.5H2O | 57.14% | Dervillite (57.14 %) |
Haidingerite | CaHAsO4 路 H2O | 57.14% | Dervillite (57.14 %) |
Lautite | CuAsS | 57.14% | Dervillite (57.14 %) |
Matildite | AgBiS2 | 57.14% | Dervillite (57.14 %) |
Mcnearite | NaCa5(AsO4)(HAsO4)4 路 4H2O | 57.14% | Dervillite (57.14 %) |
Miargyrite | AgSbS2 | 57.14% | Dervillite (57.14 %) |
Rauenthalite | Ca3(AsO4)2 路 10H2O | 57.14% | Dervillite (57.14 %) |
R枚sslerite | Mg(HAsO4) 路 7H2O | 57.14% | Dervillite (57.14 %) |
Sainfeldite | Ca5(AsO4)2(AsO3OH)2 路 4H2O | 57.14% | Dervillite (57.14 %) |
Weilite | Ca(HAsO4) | 57.14% | Dervillite (57.14 %) |
Hessite | Ag2Te | 56.79% | Coloradoite (56.80 %) |
Uranophane | Ca(UO2)2(SiO3OH)2 路 5H2O | 56.66% | Metanov谩膷ekite (56.67 %) |
Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 56.41% | Schultenite (56.41 %) |
Altaite | PbTe | 55.82% | Coloradoite (55.83 %) |
Petzite | Ag3AuTe2 | 54.85% | Coloradoite (54.85 %) |
Langite | Cu4(SO4)(OH)6 路 2H2O | 53.60% | Parnauite (53.60 %) |
Duftite | PbCu(AsO4)(OH) | 53.57% | Arsendescloizite (53.57 %) |
Montebrasite | LiAl(PO4)(OH) | 50.00% | 膶ern媒ite (50.00 %) |
Lindstr枚mite | Pb3Cu3Bi7S15 | 50.00% | Paarite (50.00 %) |
Salammoniac | NH4Cl | 50.00% | Mohrite (50.00 %) |
Hollandite | Ba(Mn4+6Mn3+2)O16 | 50.00% | Gasparite-(La) (50.00 %) |
Pyrobelonite | PbMn2+(VO4)(OH) | 50.00% | Gasparite-(La) (50.00 %) |
Pyrolusite | Mn4+O2 | 50.00% | Gasparite-(La) (50.00 %) |
Pyrophanite | Mn2+TiO3 | 50.00% | Gasparite-(La) (50.00 %) |
Richterite | Na(NaCa)Mg5(Si8O22)(OH)2 | 50.00% | Gasparite-(La) (50.00 %) |
Tephroite | Mn2+2SiO4 | 50.00% | Gasparite-(La) (50.00 %) |
Safflorite | (Co,Ni,Fe)As2 | 45.71% | Dervillite (57.14 %) |
Skutterudite | CoAs3 | 45.71% | Dervillite (57.14 %) |
Sperrylite | PtAs2 | 40.00% | Tetra-auricupride (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.