Predictive Mineralogy
Possible unrecorded species at Salsigne mine, Salsigne, Carcassonne, Aude, Occitanie, France
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 |
---|---|---|---|
Smithsonite | ZnCO3 | 100.00% | Aurichalcite (54.58 %), Yvonite (100.00 %) |
Gypsum | CaSO4 路 2H2O | 99.99% | Brandtite (52.38 %), Brassite (71.43 %), Carbonatecyanotrichite (54.76 %), Cyanotrichite (52.36 %), Devilline (67.06 %), Geminite (66.67 %), Gu茅rinite (70.27 %), Hydrowoodwardite (58.82 %), Lindackerite (72.73 %), Picropharmacolite (50.83 %), Posnjakite (58.43 %), Rauenthalite (70.00 %), Richelsdorfite (64.71 %) |
Goethite | 伪-Fe3+O(OH) | 99.98% | Arseniosiderite (52.65 %), Beudantite (54.12 %), Brandtite (52.38 %), Cornubite (54.62 %), Delafossite (65.68 %), Devilline (51.87 %), Geminite (55.56 %), Langite (50.97 %), Lindackerite (54.55 %), Parnauite (57.60 %), Z谩les铆ite (53.47 %) |
Hematite | Fe2O3 | 99.51% | Brandtite (66.67 %), Delafossite (65.09 %), Guanajuatite (51.22 %), Gu茅rinite (54.05 %), Hydrowoodwardite (58.82 %), Z谩les铆ite (54.46 %) |
Pharmacolite | Ca(HAsO4) 路 2H2O | 99.05% | Brassite (50.00 %), Gu茅rinite (75.68 %), Lindackerite (63.64 %), Picropharmacolite (50.83 %), Rauenthalite (56.67 %) |
Covellite | CuS | 98.53% | Delafossite (58.58 %), Lindackerite (63.64 %), Parnauite (56.00 %), Posnjakite (54.49 %), Richelsdorfite (51.47 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 路 nH2O, x < 1 | 96.90% | Clinoclase (52.74 %), Lindackerite (54.55 %), Parnauite (58.40 %), Z谩les铆ite (65.35 %) |
Acanthite | Ag2S | 94.99% | Lindackerite (72.73 %), Polybasite (60.65 %), Rauenthalite (53.33 %) |
Fluorite | CaF2 | 90.06% | Gu茅rinite (54.05 %), Hydrowoodwardite (52.94 %), Siderophyllite (54.05 %) |
Mimetite | Pb5(AsO4)3Cl | 89.18% | Beudantite (54.73 %), Claraite (51.02 %), Parnauite (51.20 %) |
Lavendulan | NaCaCu5(AsO4)4Cl 路 5H2O | 87.87% | Geminite (66.67 %), Lindackerite (63.64 %) |
L枚llingite | FeAs2 | 84.14% | Gu茅rinite (56.76 %), Rauenthalite (63.33 %) |
K枚ttigite | Zn3(AsO4)2 路 8H2O | 83.83% | Geminite (55.56 %), Lindackerite (63.64 %) |
Cornwallite | Cu5(AsO4)2(OH)4 | 82.32% | Clinoclase (58.22 %), Cornubite (57.69 %) |
Sainfeldite | Ca5(AsO4)2(AsO3OH)2 路 4H2O | 81.62% | Gu茅rinite (54.05 %), Rauenthalite (60.00 %) |
Erythrite | Co3(AsO4)2 路 8H2O | 79.47% | Geminite (55.56 %), Gu茅rinite (59.46 %), Lindackerite (54.55 %), Picropharmacolite (50.00 %), Rauenthalite (60.00 %), Richelsdorfite (60.29 %) |
Microcline | K(AlSi3O8) | 78.57% | Gormanite (50.00 %), Messelite (57.14 %) |
Triphylite | LiFe2+PO4 | 72.45% | Gormanite (50.00 %), Ludlamite (56.00 %), Messelite (57.14 %) |
Skutterudite | CoAs3 | 69.90% | Gu茅rinite (62.16 %), Rauenthalite (66.67 %) |
Beryl | Be3Al2(Si6O18) | 63.08% | Ludlamite (50.67 %), Messelite (57.14 %) |
Annabergite | Ni3(AsO4)2 路 8H2O | 63.03% | Lindackerite (54.55 %), Rauenthalite (53.33 %) |
Cassiterite | SnO2 | 61.83% | Stannite (61.84 %) |
Theisite | Cu5Zn5(AsO4,SbO4)2(OH)14 | 59.18% | Claraite (59.18 %) |
Rhodochrosite | MnCO3 | 57.14% | Brandtite (57.14 %) |
Arsenic | As | 56.66% | Rauenthalite (56.67 %) |
H枚rnesite | Mg3(AsO4)2 路 8H2O | 56.66% | Rauenthalite (56.67 %) |
Pyrargyrite | Ag3SbS3 | 55.83% | Polybasite (55.84 %) |
Pharmacosiderite | KFe3+4(AsO4)3(OH)4 路 6-7H2O | 55.55% | Geminite (55.56 %) |
Jarosite | KFe3+3(SO4)2(OH)6 | 54.54% | Lindackerite (54.55 %) |
Eosphorite | Mn2+Al(PO4)(OH)2 路 H2O | 53.33% | Gormanite (53.33 %) |
Beraunite | Fe3+6(PO4)4O(OH)4 路 6H2O | 53.06% | Messelite (53.06 %) |
Heterosite | (Fe3+,Mn3+)PO4 | 53.06% | Messelite (53.06 %) |
Rockbridgeite | Fe2+Fe3+4(PO4)3(OH)5 | 53.06% | Messelite (53.06 %) |
Woodwardite | Cu1-xAlx(OH)2(SO4)x/2 路 nH2O | 52.94% | Hydrowoodwardite (52.94 %) |
Pyrolusite | Mn4+O2 | 52.38% | Brandtite (52.38 %) |
Sarkinite | Mn2+2(AsO4)(OH) | 52.38% | Brandtite (52.38 %) |
Mitridatite | Ca2Fe3+3(PO4)3O2 路 3H2O | 51.02% | Messelite (51.02 %) |
Safflorite | (Co,Ni,Fe)As2 | 50.66% | Rauenthalite (63.33 %) |
Hemimorphite | Zn4Si2O7(OH)2 路 H2O | 50.46% | Aurichalcite (50.47 %) |
Montebrasite | LiAl(PO4)(OH) | 45.33% | Gormanite (56.67 %) |
Schorl | NaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH) | 44.08% | Messelite (55.10 %) |
Zircon | Zr(SiO4) | 40.00% | Gormanite (50.00 %) |
Nickelskutterudite | (Ni,Co,Fe)As3 | 40.00% | Rauenthalite (50.00 %) |
Nickeline | NiAs | 40.00% | Rauenthalite (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.