Predictive Mineralogy
Possible unrecorded species at Km 3 open pit, Km 3 mines, Km 3, Lavrion Mining District, Lavreotiki, East Attica, Attica, Greece
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 |
|---|---|---|---|
| Sphalerite | ZnS | 99.99% | Adamite (55.00 %), Anglesite (64.09 %), Ankerite (53.36 %), Annabergite (52.59 %), Arsenopyrite (55.02 %), Brochantite (50.32 %), Cerussite (56.70 %), Chalcophanite (59.28 %), Chalcopyrite (50.66 %), Coronadite (57.20 %), Duftite (51.18 %), Galena (65.95 %), Germanite (83.33 %), Gersdorffite (65.94 %), Hetaerolite (58.72 %), Marcasite (65.85 %), Millerite (50.48 %), Mimetite (53.11 %), Nickelaustinite (57.14 %), Rosasite (67.03 %), Nickeline (53.48 %), Plattnerite (51.02 %), Polydymite (59.62 %), Rammelsbergite (61.37 %), Safflorite (56.95 %), Siegenite (68.94 %), Smithsonite (72.43 %), Ullmannite (81.84 %), Vaesite (59.06 %), Zden臅kite (66.67 %), Zincolivenite (54.88 %) |
| Pyrrhotite | Fe1-xS | 97.93% | Gersdorffite (51.37 %), Polydymite (51.92 %), Ullmannite (59.50 %), Violarite (78.17 %) |
| Arseniosiderite | Ca2Fe3+3(AsO4)3O2 路 3H2O | 97.14% | Ferrilotharmeyerite (85.71 %), Nickellotharmeyerite (80.00 %) |
| Hemimorphite | Zn4Si2O7(OH)2 路 H2O | 92.20% | Hetaerolite (50.46 %), Rosasite (63.74 %), Plattnerite (56.63 %) |
| Magnetite | Fe2+Fe3+2O4 | 91.64% | Pecoraite (52.17 %), Polydymite (50.64 %), Violarite (64.59 %) |
| Scorodite | Fe3+AsO4 路 2H2O | 89.01% | Arthurite (74.36 %), Ferrilotharmeyerite (57.14 %) |
| Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 路 nH2O, x < 1 | 88.23% | Conichalcite (50.59 %), Duftite (51.18 %), Zincolivenite (51.22 %) |
| Copper | Cu | 83.76% | Arthurite (51.28 %), Zden臅kite (66.67 %) |
| Uraninite | UO2 | 83.39% | Heinrichite (57.14 %), Johannite (61.25 %) |
| Skutterudite | CoAs3 | 80.57% | Rammelsbergite (53.43 %), Safflorite (58.29 %) |
| Pentlandite | (NixFey)危9S8 | 79.06% | Violarite (79.06 %) |
| Zeunerite | Cu(UO2)2(AsO4)2 路 12H2O | 66.66% | Heinrichite (66.67 %) |
| Chalcanthite | CuSO4 路 5H2O | 66.66% | Zden臅kite (66.67 %) |
| Zippeite | K3(UO2)4(SO4)2O3(OH) 路 3H2O | 65.00% | Johannite (65.00 %) |
| Bornite | Cu5FeS4 | 64.28% | Germanite (64.29 %) |
| Pharmacosiderite | KFe3+4(AsO4)3(OH)4 路 6-7H2O | 61.53% | Arthurite (61.54 %) |
| Atacamite | Cu2(OH)3Cl | 60.71% | Clinoatacamite (60.71 %) |
| Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 59.34% | Rosasite (59.34 %) |
| Aegirine | NaFe3+Si2O6 | 59.09% | Wallkilldellite (59.09 %) |
| Rhodonite | CaMn3Mn[Si5O15] | 59.09% | Wallkilldellite (59.09 %) |
| Jarosite | KFe3+3(SO4)2(OH)6 | 58.97% | Arthurite (58.97 %) |
| Erythrite | Co3(AsO4)2 路 8H2O | 57.76% | Annabergite (57.77 %) |
| Chalcocite | Cu2S | 57.14% | Ferrilotharmeyerite (57.14 %) |
| Mawbyite | PbFe3+2(AsO4)2(OH)2 | 57.14% | Ferrilotharmeyerite (57.14 %) |
| Metazeunerite | Cu(UO2)2(AsO4)2 路 8H2O | 57.14% | Ferrilotharmeyerite (57.14 %) |
| Cobaltlotharmeyerite | CaCo2(AsO4)2 路 2H2O | 57.14% | Ferrilotharmeyerite (57.14 %) |
| L枚llingite | FeAs2 | 57.14% | Nickelaustinite (57.14 %) |
| Torbernite | Cu(UO2)2(PO4)2 路 12H2O | 56.25% | Johannite (56.25 %) |
| Albite | Na(AlSi3O8) | 54.54% | Wallkilldellite (54.55 %) |
| Braunite | Mn2+Mn3+6(SiO4)O8 | 54.54% | Wallkilldellite (54.55 %) |
| Manganite | Mn3+O(OH) | 53.84% | Groutite (53.85 %) |
| Chlorargyrite | AgCl | 53.33% | Zden臅kite (66.67 %) |
| Uranophane | Ca(UO2)2(SiO3OH)2 路 5H2O | 52.38% | Heinrichite (52.38 %) |
| Kutnohorite | CaMn2+(CO3)2 | 50.00% | Wallkilldellite (50.00 %) |
| Manganberzeliite | (NaCa2)Mn2+2(AsO4)3 | 50.00% | Wallkilldellite (50.00 %) |
| Rhodochrosite | MnCO3 | 50.00% | Wallkilldellite (50.00 %) |
| Silver | Ag | 47.70% | Safflorite (59.63 %) |
| Gold | Au | 41.90% | Germanite (52.38 %) |
| Zircon | Zr(SiO4) | 40.00% | Hydroxycalciorom茅ite (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.