Predictive Mineralogy
Possible unrecorded species at Tennvatn pegmatite, S酶rfold, Nordland, Norway
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 |
---|---|---|---|
Pyrite | FeS2 | 100.00% | Aikinite (81.56 %), Anatase (53.26 %), Anglesite (64.19 %), Antlerite (70.31 %), Arsenocrandallite (75.00 %), Asbecasite (55.56 %), Bastn盲site-(Ce) (53.63 %), Bayldonite (57.79 %), Bismoclite (61.63 %), Bismuth (65.41 %), Bismuthinite (76.49 %), Calcioancylite-(Ce) (62.26 %), Calcite (51.16 %), Cannizzarite (84.78 %), Cerussite (56.77 %), Chalcanthite (74.95 %), Clinochlore (51.79 %), Cosalite (82.49 %), Covellite (80.77 %), Fassinaite (66.67 %), Friedrichite (76.92 %), Galena (66.84 %), Greenockite (76.91 %), Hematite (50.17 %), Hingganite-(Y) (64.18 %), Hydrocerussite (53.78 %), Kasolite (50.68 %), Krupkaite (82.47 %), Lindstr枚mite (80.43 %), L枚llingite (66.48 %), Mimetite (59.01 %), Mixite (52.60 %), Muscovite (50.01 %), Nuffieldite (76.32 %), Pekoite (84.44 %), Pharmacosiderite (64.43 %), Philipsbornite (69.35 %), Preisingerite (63.93 %), Rutile (52.79 %), Stibarsen (67.21 %), Sulphur (55.07 %), Yukonite (55.88 %), Zavaritskite (62.86 %) |
Chalcopyrite | CuFeS2 | 100.00% | Aikinite (85.19 %), Anglesite (58.14 %), Antlerite (73.04 %), Arsenocrandallite (75.00 %), Bayldonite (68.84 %), Bismoclite (51.16 %), Bismuth (65.27 %), Bismuthinite (73.84 %), Cannizzarite (71.74 %), Chalcanthite (74.56 %), Cosalite (79.19 %), Covellite (85.83 %), Fassinaite (66.67 %), Friedrichite (78.85 %), Galena (56.79 %), Greenockite (68.77 %), Hydrocerussite (53.78 %), Krupkaite (78.35 %), Lindstr枚mite (78.26 %), L枚llingite (64.20 %), Mimetite (52.87 %), Mixite (63.02 %), Nuffieldite (76.32 %), Pekoite (84.44 %), Perite (53.66 %), Pharmacosiderite (59.35 %), Philipsbornite (59.68 %), Preisingerite (62.30 %), Stibarsen (62.30 %), Susannite (61.74 %), Yukonite (58.82 %), Zavaritskite (68.57 %) |
Malachite | Cu2(CO3)(OH)2 | 99.99% | Anglesite (50.35 %), Antlerite (71.67 %), Arsenocrandallite (87.50 %), Asbecasite (66.67 %), Bayldonite (80.90 %), Chalcanthite (62.86 %), Covellite (54.66 %), Fassinaite (86.67 %), Hydrocerussite (63.11 %), Mimetite (60.02 %), Mixite (70.31 %), Philipsbornite (64.52 %), Phosgenite (50.91 %), Preisingerite (50.82 %), Susannite (79.13 %), Yukonite (50.00 %) |
Goethite | 伪-Fe3+O(OH) | 99.98% | Arsenocrandallite (75.00 %), Bayldonite (53.77 %), Fassinaite (73.33 %), Hydrocerussite (53.33 %), Mixite (51.04 %), Perite (65.85 %), Philipsbornite (59.68 %), Susannite (61.74 %), Yukonite (50.00 %) |
Arsenopyrite | FeAsS | 99.97% | Arsenocrandallite (62.50 %), Cannizzarite (52.17 %), Cosalite (55.33 %), L枚llingite (65.68 %), Pharmacosiderite (58.74 %), Philipsbornite (58.06 %), Preisingerite (50.82 %), Yukonite (64.71 %), Zavaritskite (71.43 %) |
Azurite | Cu3(CO3)2(OH)2 | 99.84% | Antlerite (55.97 %), Arsenocrandallite (87.50 %), Bayldonite (66.83 %), Fassinaite (60.00 %), Mixite (54.17 %), Philipsbornite (54.84 %) |
Brochantite | Cu4(SO4)(OH)6 | 99.45% | Antlerite (70.65 %), Arsenocrandallite (68.75 %), Bayldonite (57.29 %), Fassinaite (66.67 %), Susannite (58.26 %) |
Scorodite | Fe3+AsO4 路 2H2O | 99.11% | Arsenocrandallite (62.50 %), Pharmacosiderite (61.99 %), Philipsbornite (58.06 %), Preisingerite (63.93 %), Yukonite (58.82 %) |
Braunite | Mn2+Mn3+6(SiO4)O8 | 97.88% | Bergslagite (55.56 %), Gasparite-(La) (87.50 %), Svabite (61.90 %) |
Linarite | PbCu(SO4)(OH)2 | 92.34% | Fassinaite (73.33 %), Susannite (71.30 %) |
Tilasite | CaMg(AsO4)F | 88.88% | Bergslagite (55.56 %), Gasparite-(La) (75.00 %) |
Olivenite | Cu2(AsO4)(OH) | 88.06% | Arsenocrandallite (75.00 %), Bayldonite (52.26 %) |
Langite | Cu4(SO4)(OH)6 路 2H2O | 87.01% | Fassinaite (73.33 %), Susannite (51.30 %) |
Cuprite | Cu2O | 81.82% | Antlerite (51.54 %), Arsenocrandallite (62.50 %) |
Aragonite | CaCO3 | 80.55% | Arsenocrandallite (56.25 %), Bergslagite (55.56 %) |
Sphalerite | ZnS | 79.99% | Aikinite (76.10 %), Anglesite (64.09 %), Antlerite (54.95 %), Arsenocrandallite (56.25 %), Bayldonite (55.28 %), Bismoclite (52.33 %), Bismuth (53.21 %), Bismuthinite (60.27 %), Cannizzarite (71.74 %), Cerussite (56.70 %), Chalcanthite (54.35 %), Cosalite (75.89 %), Covellite (64.68 %), Fassinaite (66.67 %), Friedrichite (61.54 %), Galena (65.95 %), Greenockite (88.40 %), Hydrocerussite (54.22 %), Krupkaite (64.95 %), Lindstr枚mite (69.57 %), L枚llingite (59.55 %), Mimetite (53.11 %), Nuffieldite (68.42 %), Pekoite (71.11 %), Philipsbornite (58.06 %), Stibarsen (59.02 %), Susannite (60.00 %), Zavaritskite (65.71 %) |
Baryte | BaSO4 | 79.62% | Arsenocrandallite (62.50 %), Bayldonite (55.28 %), Bergslagite (66.67 %), Fassinaite (60.00 %), Gasparite-(La) (50.00 %), Mixite (57.81 %) |
Pyrrhotite | Fe1-xS | 78.92% | Cannizzarite (56.52 %), Cosalite (51.52 %) |
Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 78.83% | Arsenocrandallite (56.25 %), Philipsbornite (51.61 %) |
Chalcocite | Cu2S | 78.25% | Arsenocrandallite (56.25 %), Covellite (50.30 %) |
Gold | Au | 77.30% | Aikinite (52.99 %), Asbecasite (55.56 %), Krupkaite (61.86 %), Pekoite (57.78 %) |
Conichalcite | CaCu(AsO4)(OH) | 68.75% | Arsenocrandallite (68.75 %) |
Cafarsite | Ca5.9Mn1.7Fe3Ti3(AsO3)12 路 4-5H2O | 66.66% | Asbecasite (66.67 %) |
Epidote | (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH) | 66.66% | Asbecasite (66.67 %) |
Uraninite | UO2 | 65.15% | Kasolite (65.16 %) |
Stibiotantalite | Sb(Ta,Nb)O4 | 62.50% | Stibiocolumbite (62.50 %) |
Aegirine | NaFe3+Si2O6 | 62.50% | Gasparite-(La) (62.50 %) |
Hausmannite | Mn2+Mn3+2O4 | 62.50% | Gasparite-(La) (62.50 %) |
Phlogopite | KMg3(AlSi3O10)(OH)2 | 62.50% | Gasparite-(La) (62.50 %) |
Rhodochrosite | MnCO3 | 62.50% | Gasparite-(La) (62.50 %) |
Rhodonite | CaMn3Mn[Si5O15] | 62.50% | Gasparite-(La) (62.50 %) |
Talc | Mg3Si4O10(OH)2 | 62.50% | Gasparite-(La) (62.50 %) |
Uranophane | Ca(UO2)2(SiO3OH)2 路 5H2O | 60.18% | Kasolite (60.18 %) |
Caledonite | Pb5Cu2(SO4)3(CO3)(OH)6 | 58.26% | Susannite (58.26 %) |
Pyromorphite | Pb5(PO4)3Cl | 57.39% | Susannite (57.39 %) |
Allophane | (Al2O3)(SiO2)1.3-2 路 2.5-3H2O | 56.25% | Arsenocrandallite (56.25 %) |
Arseniosiderite | Ca2Fe3+3(AsO4)3O2 路 3H2O | 56.25% | Arsenocrandallite (56.25 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 路 nH2O, x < 1 | 56.25% | Arsenocrandallite (56.25 %) |
Cornwallite | Cu5(AsO4)2(OH)4 | 56.25% | Arsenocrandallite (56.25 %) |
Jarosite | KFe3+3(SO4)2(OH)6 | 56.25% | Arsenocrandallite (56.25 %) |
Siderite | FeCO3 | 56.25% | Arsenocrandallite (56.25 %) |
Arsenic | As | 55.73% | Stibarsen (55.74 %) |
Gladite | PbCuBi5S9 | 55.55% | Pekoite (55.56 %) |
Synchysite-(Ce) | CaCe(CO3)2F | 55.55% | Asbecasite (55.56 %) |
Adamite | Zn2(AsO4)(OH) | 55.00% | Arsenocrandallite (68.75 %) |
Stibnite | Sb2S3 | 54.09% | Stibarsen (54.10 %) |
Gadolinite-(Y) | Y2Fe2+Be2Si2O10 | 53.33% | Tengerite-(Y) (53.33 %) |
Bornite | Cu5FeS4 | 53.33% | Fassinaite (53.33 %) |
Devilline | CaCu4(SO4)2(OH)6 路 3H2O | 53.33% | Fassinaite (53.33 %) |
Leadhillite | Pb4(CO3)2(SO4)(OH)2 | 53.04% | Susannite (53.04 %) |
Hammarite | Pb2Cu2Bi4S9 | 52.17% | Lindstr枚mite (52.17 %) |
Carminite | PbFe3+2(AsO4)2(OH)2 | 50.00% | Arsenocrandallite (50.00 %) |
Connellite | Cu19(SO4)(OH)32Cl4 路 3H2O | 50.00% | Arsenocrandallite (50.00 %) |
Cornubite | Cu5(AsO4)2(OH)4 | 50.00% | Arsenocrandallite (50.00 %) |
Copper | Cu | 50.00% | Arsenocrandallite (50.00 %) |
Lavendulan | NaCaCu5(AsO4)4Cl 路 5H2O | 50.00% | Arsenocrandallite (50.00 %) |
Marcasite | FeS2 | 50.00% | Arsenocrandallite (50.00 %) |
Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) | 50.00% | Stibiocolumbite (62.50 %) |
Piemontite | (CaCa)(AlAlMn3+)O[Si2O7][SiO4](OH) | 50.00% | Gasparite-(La) (50.00 %) |
Pyrolusite | Mn4+O2 | 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 %) |
Todorokite | (Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 路 3-4H2O | 50.00% | Gasparite-(La) (50.00 %) |
Hemimorphite | Zn4Si2O7(OH)2 路 H2O | 42.43% | Susannite (53.04 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 40.00% | Arsenocrandallite (50.00 %) |
Smithsonite | ZnCO3 | 40.00% | Arsenocrandallite (50.00 %) |
Hollandite | Ba(Mn4+6Mn3+2)O16 | 40.00% | Gasparite-(La) (50.00 %) |
Pyrobelonite | PbMn2+(VO4)(OH) | 40.00% | Gasparite-(La) (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.