Predictive Mineralogy
Possible unrecorded species at Lead and silver smelter slag locality, Braubach, Loreley, Rhein-Lahn-Kreis, Rhineland-Palatinate, 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 |
---|---|---|---|
Quartz | SiO2 | 99.99% | Anglesite (68.30 %), Aragonite (53.70 %), Brochantite (70.20 %), Calcite (62.43 %), Cerussite (63.56 %), Chalconatronite (68.00 %), Copper (56.56 %), Covellite (76.39 %), Cristobalite (57.14 %), Cuprite (65.19 %), Elyite (50.54 %), H枚rnesite (77.60 %), Ktenasite (78.26 %), Langite (78.01 %), Linarite (74.40 %), Malachite (61.21 %), Namuwite (72.60 %), Natrojarosite (65.92 %), Olivenite (72.44 %), Plumbonacrite (64.29 %), Posnjakite (73.88 %), Serpierite (72.17 %), Spertiniite (72.73 %), Strashimirite (78.26 %), Zincite (53.70 %) |
Galena | PbS | 99.99% | Anglesite (86.19 %), Brochantite (55.97 %), Cerussite (83.05 %), Covellite (64.18 %), Elyite (68.82 %), H枚rnesite (58.40 %), Ktenasite (85.87 %), Langite (63.00 %), Laurionite (75.86 %), Linarite (83.08 %), Litharge (59.51 %), Namuwite (78.08 %), Olivenite (50.95 %), Plumbonacrite (71.43 %), Posnjakite (59.83 %), Serpierite (74.78 %), Spertiniite (63.64 %), Strashimirite (54.78 %), Zincite (58.33 %) |
Chalcopyrite | CuFeS2 | 99.99% | Anglesite (58.14 %), Brochantite (71.06 %), Copper (53.15 %), Covellite (85.83 %), Cuprite (67.05 %), H枚rnesite (68.80 %), Ktenasite (79.35 %), Langite (78.16 %), Linarite (69.97 %), Malachite (60.66 %), Namuwite (67.12 %), Olivenite (65.16 %), Plumbonacrite (64.29 %), Posnjakite (77.25 %), Serpierite (75.36 %), Spertiniite (68.18 %), Strashimirite (75.65 %) |
Pyrite | FeS2 | 99.99% | Anglesite (64.19 %), Brochantite (63.33 %), Calcite (51.16 %), Cerussite (56.77 %), Covellite (80.77 %), Cuprite (58.26 %), Dypingite (52.63 %), H枚rnesite (72.00 %), Ktenasite (75.00 %), Langite (68.50 %), Linarite (63.77 %), Malachite (52.79 %), Namuwite (63.01 %), Natrojarosite (64.63 %), Olivenite (56.33 %), Plumbonacrite (50.00 %), Posnjakite (70.22 %), Serpierite (71.30 %), Spertiniite (54.55 %), Strashimirite (62.61 %), Zincite (51.85 %) |
Sphalerite | ZnS | 99.99% | Anglesite (64.09 %), Brochantite (50.32 %), Cerussite (56.70 %), Covellite (64.68 %), H枚rnesite (52.80 %), Ktenasite (79.35 %), Langite (58.40 %), Linarite (66.52 %), Namuwite (75.34 %), Plumbonacrite (57.14 %), Posnjakite (55.90 %), Serpierite (70.43 %), Spertiniite (59.09 %), Zincite (61.11 %) |
Goethite | 伪-Fe3+O(OH) | 99.95% | Elyite (59.14 %), Ktenasite (66.30 %), Langite (50.97 %), Laurionite (58.62 %), Namuwite (63.01 %), Plumbonacrite (50.00 %), Serpierite (51.59 %), Spertiniite (59.09 %), Strashimirite (54.78 %) |
Azurite | Cu3(CO3)2(OH)2 | 99.82% | Cuprite (51.54 %), Ktenasite (53.26 %), Langite (53.49 %), Olivenite (66.38 %), Posnjakite (58.15 %), Serpierite (51.01 %), Strashimirite (76.52 %) |
Hematite | Fe2O3 | 97.88% | Ktenasite (56.52 %), Piypite (75.00 %), Plumbonacrite (57.14 %), Spertiniite (54.55 %) |
Magnetite | Fe2+Fe3+2O4 | 95.00% | Nyerereite (80.00 %), Plumbonacrite (50.00 %), Spertiniite (50.00 %) |
Hydrocerussite | Pb3(CO3)2(OH)2 | 90.65% | Elyite (61.29 %), Laurionite (51.72 %), Plumbonacrite (50.00 %) |
Euchlorine | KNaCu3(SO4)3O | 87.50% | Piypite (87.50 %) |
Tenorite | CuO | 87.50% | Piypite (87.50 %) |
Smithsonite | ZnCO3 | 87.13% | Ktenasite (65.22 %), Namuwite (63.01 %) |
Dolomite | CaMg(CO3)2 | 86.50% | H枚rnesite (63.20 %), Nyerereite (63.33 %) |
Halite | NaCl | 84.85% | Piypite (62.50 %), Trona (59.62 %) |
Hydrozincite | Zn5(CO3)2(OH)6 | 81.90% | Ktenasite (51.09 %), Namuwite (63.01 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 80.13% | Ktenasite (50.00 %), Namuwite (60.27 %) |
Hemimorphite | Zn4Si2O7(OH)2 路 H2O | 79.09% | Ktenasite (57.61 %), Namuwite (50.68 %) |
Baryte | BaSO4 | 77.41% | Ktenasite (56.52 %), Namuwite (50.68 %), Nyerereite (56.67 %), Strashimirite (65.22 %) |
Chalcocite | Cu2S | 77.41% | Covellite (50.30 %), Spertiniite (54.55 %) |
Dolerophanite | Cu2(SO4)O | 75.00% | Piypite (75.00 %) |
Melanothallite | Cu2Cl2O | 75.00% | Piypite (75.00 %) |
Schulenbergite | (Cu,Zn)7(SO4)2(OH)10 路 3H2O | 65.75% | Namuwite (65.75 %) |
Caledonite | Pb5Cu2(SO4)3(CO3)(OH)6 | 64.51% | Elyite (64.52 %) |
Phosgenite | Pb2CO3Cl2 | 63.79% | Laurionite (63.79 %) |
Phlogopite | KMg3(AlSi3O10)(OH)2 | 63.33% | Nyerereite (63.33 %) |
Chalcocyanite | CuSO4 | 62.50% | Piypite (62.50 %) |
Cotunnite | PbCl2 | 62.50% | Piypite (62.50 %) |
Sylvite | KCl | 62.50% | Piypite (62.50 %) |
Th茅nardite | Na2SO4 | 62.50% | Piypite (62.50 %) |
Nepheline | Na3K(Al4Si4O16) | 60.00% | Nyerereite (60.00 %) |
Tyrolite | Ca2Cu9(AsO4)4(CO3)(OH)8 路 11H2O | 57.39% | Strashimirite (57.39 %) |
Diopside | CaMgSi2O6 | 56.66% | Nyerereite (56.67 %) |
Pyrrhotite | Fe1-xS | 56.66% | Nyerereite (56.67 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 路 nH2O, x < 1 | 55.65% | Strashimirite (55.65 %) |
Sulphur | S8 | 54.79% | Namuwite (54.79 %) |
Forsterite | Mg2SiO4 | 53.33% | Nyerereite (53.33 %) |
Mimetite | Pb5(AsO4)3Cl | 52.17% | Ktenasite (52.17 %) |
Arsenopyrite | FeAsS | 52.00% | H枚rnesite (52.00 %) |
Paralaurionite | PbCl(OH) | 51.72% | Laurionite (51.72 %) |
Lanarkite | Pb2(SO4)O | 51.61% | Elyite (51.61 %) |
Leadhillite | Pb4(CO3)2(SO4)(OH)2 | 51.61% | Elyite (51.61 %) |
Perovskite | CaTiO3 | 50.66% | Nyerereite (63.33 %) |
Monticellite | CaMgSiO4 | 50.00% | Nyerereite (50.00 %) |
Anhydrite | CaSO4 | 50.00% | Piypite (50.00 %) |
Aphthitalite | (K,Na)3Na(SO4)2 | 50.00% | Piypite (50.00 %) |
Cyanochroite | K2Cu(SO4)2 路 6H2O | 50.00% | Piypite (50.00 %) |
Hydrokenoralstonite | Na0.5(Al,Mg)2(F,OH)6 路 H2O | 50.00% | Piypite (50.00 %) |
Sellaite | MgF2 | 50.00% | Piypite (50.00 %) |
Erythrite | Co3(AsO4)2 路 8H2O | 41.60% | H枚rnesite (52.00 %) |
Ilmenite | Fe2+TiO3 | 40.00% | Nyerereite (50.00 %) |
Titanite | CaTi(SiO4)O | 40.00% | Nyerereite (50.00 %) |
Sofiite | Zn2(SeO3)Cl2 | 40.00% | Piypite (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.