Predictive Mineralogy
Possible unrecorded species at Neubulach, Calw, Karlsruhe Region, Baden-Württemberg, Germany
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 |
---|---|---|---|
Galena | PbS | 99.99% | Adamite (66.33 %), Agardite-(Ce) (77.08 %), Ankerite (54.09 %), Arseniosiderite (52.21 %), Arsenocrandallite (68.75 %), Bariopharmacosiderite (53.23 %), Bayldonite (74.37 %), Brochantite (55.97 %), Chalcophyllite (55.56 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Cyanotrichite (57.08 %), Digenite (59.98 %), Emplectite (61.38 %), Ferrisymplesite (50.00 %), Langite (63.00 %), Olivenite (50.95 %), Parnauite (60.80 %), Philipsburgite (60.61 %), Pitticite (62.67 %), Pyromorphite (77.81 %), Rooseveltite (52.27 %), Spionkopite (58.14 %), Strashimirite (54.78 %), Yarrowite (51.81 %), Zincolivenite (75.61 %) |
Sphalerite | ZnS | 99.99% | Adamite (55.00 %), Agardite-(Ce) (62.50 %), Ankerite (53.36 %), Arsenocrandallite (56.25 %), Bayldonite (55.28 %), Brochantite (50.32 %), Chalcophyllite (54.67 %), Chalcopyrite (50.66 %), Covellite (64.68 %), Digenite (61.34 %), Emplectite (62.41 %), Ferrisymplesite (58.33 %), Langite (58.40 %), Mansfieldite (54.17 %), Parnauite (50.40 %), Philipsburgite (60.61 %), Pitticite (60.00 %), Pyromorphite (56.90 %), Rooseveltite (56.82 %), Spionkopite (67.44 %), Yarrowite (65.06 %), Zincolivenite (54.88 %) |
Cerussite | PbCO3 | 99.99% | Adamite (60.00 %), Agardite-(Ce) (62.50 %), Arsenocrandallite (62.50 %), Bayldonite (73.37 %), Cyanotrichite (50.47 %), Langite (53.94 %), Parnauite (51.20 %), Philipsburgite (63.64 %), Pyromorphite (68.61 %), Zincolivenite (58.54 %) |
Arsenopyrite | FeAsS | 99.94% | Arsenocrandallite (62.50 %), Bulachite (80.00 %), Ferrisymplesite (54.17 %), Mansfieldite (66.67 %), Pitticite (66.67 %), Preisingerite (50.82 %), Rooseveltite (68.18 %) |
Scorodite | Fe3+AsO4 · 2H2O | 99.91% | Arseniosiderite (57.52 %), Arsenocrandallite (62.50 %), Ferrisymplesite (62.50 %), Mansfieldite (70.83 %), Pitticite (50.67 %), Preisingerite (63.93 %), Rooseveltite (72.73 %) |
Mimetite | Pb5(AsO4)3Cl | 99.90% | Adamite (58.67 %), Agardite-(Ce) (64.58 %), Arsenocrandallite (56.25 %), Bayldonite (71.86 %), Parnauite (51.20 %), Philipsburgite (69.70 %), Zincolivenite (65.85 %) |
Gypsum | CaSO4 · 2H2O | 96.43% | Arsenocrandallite (68.75 %), Bariopharmacoalumite (50.00 %), Cyanotrichite (52.36 %), Strashimirite (52.17 %) |
Bismuthinite | Bi2S3 | 94.13% | Emplectite (57.24 %), Preisingerite (62.30 %), Rooseveltite (63.64 %) |
Anglesite | PbSO4 | 94.03% | Agardite-(Ce) (50.00 %), Arsenocrandallite (50.00 %), Bayldonite (52.26 %), Zincolivenite (50.00 %) |
Bismuth | Bi | 93.29% | Ferrisymplesite (50.00 %), Preisingerite (60.66 %), Rooseveltite (65.91 %) |
Aragonite | CaCO3 | 83.59% | Arsenocrandallite (56.25 %), Ferrisymplesite (62.50 %) |
Smithsonite | ZnCO3 | 76.82% | Arsenocrandallite (50.00 %), Zincolivenite (53.66 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 75.75% | Arsenocrandallite (50.00 %), Philipsburgite (51.52 %) |
Lavendulan | NaCaCu5(AsO4)4Cl · 5H2O | 75.00% | Arsenocrandallite (50.00 %), Bariopharmacoalumite (50.00 %) |
Pharmacosiderite | KFe3+4(AsO4)3(OH)4 · 6-7H2O | 62.50% | Arsenocrandallite (62.50 %) |
Silver | Ag | 60.00% | Agardite-(Ce) (50.00 %), Ferrisymplesite (50.00 %) |
Duftite | PbCu(AsO4)(OH) | 57.57% | Philipsburgite (57.58 %) |
Beudantite | PbFe3(AsO4)(SO4)(OH)6 | 56.25% | Arsenocrandallite (56.25 %) |
Hemimorphite | Zn4Si2O7(OH)2 · H2O | 54.54% | Philipsburgite (54.55 %) |
Linarite | PbCu(SO4)(OH)2 | 52.08% | Agardite-(Ce) (52.08 %) |
Autunite | Ca(UO2)2(PO4)2 · 10-12H2O | 51.51% | Torbernite (51.52 %) |
Löllingite | FeAs2 | 50.00% | Ferrisymplesite (50.00 %) |
Parasymplesite | Fe2+3(AsO4)2 · 8H2O | 50.00% | Ferrisymplesite (50.00 %) |
Carminite | PbFe3+2(AsO4)2(OH)2 | 50.00% | Arsenocrandallite (50.00 %) |
Connellite | Cu19(SO4)(OH)32Cl4 · 3H2O | 50.00% | Arsenocrandallite (50.00 %) |
Marcasite | FeS2 | 50.00% | Arsenocrandallite (50.00 %) |
Sulphur | S8 | 50.00% | Arsenocrandallite (50.00 %) |
Erythrite | Co3(AsO4)2 · 8H2O | 43.33% | Ferrisymplesite (54.17 %) |
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.