Predictive Mineralogy
Possible unrecorded species at Baños de Alhamilla, Pechina, Almería, Andalusia, Spain
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 |
---|---|---|---|
Arsenopyrite | FeAsS | 99.99% | Argentopyrite (50.75 %), Bournonite (55.79 %), Chalcostibite (60.68 %), Freieslebenite (57.72 %), Fülöppite (75.76 %), Heteromorphite (68.18 %), Hörnesite (52.00 %), Miargyrite (53.57 %), Plagionite (69.03 %), Ramdohrite (85.00 %), Robinsonite (56.60 %), Rösslerite (56.52 %), Scorodite (74.10 %), Semseyite (59.91 %), Senarmontite (52.66 %), Twinnite (84.00 %), Veenite (66.67 %), Zinkenite (59.48 %) |
Azurite | Cu3(CO3)2(OH)2 | 99.99% | Adamite (59.67 %), Antlerite (55.97 %), Beaverite-(Cu) (65.27 %), Carbonatecyanotrichite (65.48 %), Chenevixite (63.55 %), Claraite (91.84 %), Connellite (50.86 %), Cornwallite (71.77 %), Cuprite (51.54 %), Devilline (58.64 %), Gordaite (54.55 %), Lavendulan (52.05 %), Olivenite (66.38 %), Ramsbeckite (50.00 %), Serpierite (51.01 %) |
Marcasite | FeS2 | 99.96% | Argentopyrite (53.73 %), Fülöppite (63.64 %), Gordaite (54.55 %), Heteromorphite (50.00 %), Klebelsbergite (50.00 %), Mopungite (77.78 %), Plagionite (56.64 %), Ramdohrite (65.00 %), Semseyite (50.47 %) |
Boulangerite | Pb5Sb4S11 | 99.95% | Geocronite (59.24 %), Heteromorphite (61.36 %), Plagionite (52.21 %), Ramdohrite (55.00 %), Robinsonite (58.49 %), Semseyite (60.38 %), Twinnite (80.00 %), Veenite (58.33 %) |
Linarite | PbCu(SO4)(OH)2 | 99.89% | Beaverite-(Cu) (52.10 %), Lanarkite (62.61 %), Mallestigite (66.67 %), Ramsbeckite (81.58 %), Schulenbergite (74.84 %), Serpierite (61.45 %) |
Pyrargyrite | Ag3SbS3 | 99.87% | Argentopyrite (59.70 %), Freieslebenite (62.60 %), Miargyrite (70.05 %), Pyrostilpnite (82.29 %), Ramdohrite (67.50 %), Rösslerite (52.17 %) |
Hematite | Fe2O3 | 99.61% | Antlerite (51.19 %), Chenevixite (50.47 %), Hedyphane (62.50 %), Lepidocrocite (55.13 %), Rösslerite (52.17 %), Spertiniite (54.55 %), Tripuhyite (55.95 %) |
Valentinite | Sb2O3 | 99.12% | Klebelsbergite (75.00 %), Mopungite (88.89 %), Senarmontite (68.60 %) |
Copper | Cu | 96.53% | Connellite (59.48 %), Manganohörnesite (54.55 %), Ramsbeckite (53.95 %), Spertiniite (59.09 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 96.46% | Heteromorphite (56.82 %), Manganohörnesite (63.64 %), Ramdohrite (55.00 %), Veenite (50.00 %) |
Langite | Cu4(SO4)(OH)6 · 2H2O | 96.17% | Mallestigite (66.67 %), Ramsbeckite (71.05 %), Schulenbergite (60.38 %) |
Smithsonite | ZnCO3 | 92.94% | Gordaite (50.00 %), Ramsbeckite (68.42 %), Schulenbergite (55.35 %) |
Aurichalcite | (Zn,Cu)5(CO3)2(OH)6 | 92.09% | Claraite (51.02 %), Ramsbeckite (65.79 %), Schulenbergite (52.83 %) |
Jamesonite | Pb4FeSb6S14 | 90.50% | Fülöppite (50.00 %), Heteromorphite (56.82 %), Twinnite (56.00 %) |
Siderite | FeCO3 | 88.63% | Heteromorphite (52.27 %), Nadorite (52.38 %), Veenite (50.00 %) |
Hydrozincite | Zn5(CO3)2(OH)6 | 86.67% | Ramsbeckite (69.74 %), Schulenbergite (55.97 %) |
Halotrichite | FeAl2(SO4)4 · 22H2O | 85.63% | Aluminocopiapite (56.90 %), Ferrinatrite (66.67 %) |
Posnjakite | Cu4(SO4)(OH)6 · H2O | 84.64% | Mallestigite (66.67 %), Ramsbeckite (53.95 %) |
Copiapite | Fe2+Fe3+4(SO4)6(OH)2 · 20H2O | 82.06% | Aluminocopiapite (55.17 %), Ferrinatrite (60.00 %) |
Nickeline | NiAs | 81.84% | Nickelskutterudite (58.25 %), Rösslerite (56.52 %) |
Realgar | As4S4 | 80.67% | Mopungite (55.56 %), Rösslerite (56.52 %) |
Stephanite | Ag5SbS4 | 80.41% | Argentopyrite (58.21 %), Pyrostilpnite (53.13 %) |
Pyrrhotite | Fe1-xS | 80.33% | Argentopyrite (53.73 %), Ramdohrite (57.50 %) |
Fluorite | CaF2 | 79.79% | Mopungite (55.56 %), Rosiaite (54.55 %) |
Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 | 77.86% | Chenevixite (53.27 %), Cornwallite (52.63 %) |
Magnetite | Fe2+Fe3+2O4 | 77.63% | Mcguinnessite (55.26 %), Spertiniite (50.00 %) |
Gold | Au | 77.49% | Heteromorphite (61.36 %), Klebelsbergite (55.00 %), Tripuhyite (50.00 %), Twinnite (64.00 %) |
Chalcocite | Cu2S | 77.41% | Covellite (50.30 %), Spertiniite (54.55 %) |
Erythrite | Co3(AsO4)2 · 8H2O | 76.74% | Annabergite (57.77 %), Hörnesite (52.00 %), Manganohörnesite (54.55 %), Nickelskutterudite (55.83 %) |
Pharmacolite | Ca(HAsO4) · 2H2O | 69.56% | Rösslerite (69.57 %) |
Hydromagnesite | Mg5(CO3)4(OH)2 · 4H2O | 66.66% | Artinite (66.67 %) |
Skutterudite | CoAs3 | 65.64% | Nickelskutterudite (58.74 %), Rösslerite (56.52 %) |
Picropharmacolite | Ca4Mg(AsO4)2(HAsO4)2 · 11H2O | 65.21% | Rösslerite (65.22 %) |
Proustite | Ag3AsS3 | 65.21% | Rösslerite (65.22 %) |
Rhodochrosite | MnCO3 | 63.63% | Manganohörnesite (63.64 %) |
Leadhillite | Pb4(CO3)2(SO4)(OH)2 | 63.47% | Lanarkite (63.48 %) |
Tyrolite | Ca2Cu9(AsO4)4(CO3)(OH)8 · 11H2O | 61.22% | Claraite (61.22 %) |
Metavoltine | K2Na6Fe2+Fe3+6O2(SO4)12 · 18H2O | 60.00% | Ferrinatrite (60.00 %) |
Hemimorphite | Zn4Si2O7(OH)2 · H2O | 59.21% | Ramsbeckite (59.21 %) |
Theisite | Cu5Zn5(AsO4,SbO4)2(OH)14 | 59.18% | Claraite (59.18 %) |
Phosgenite | Pb2CO3Cl2 | 57.14% | Cumengeite (57.14 %) |
Tamarugite | NaAl(SO4)2 · 6H2O | 56.66% | Ferrinatrite (56.67 %) |
Arsenolite | As2O3 | 56.52% | Rösslerite (56.52 %) |
Arsenic | As | 56.52% | Rösslerite (56.52 %) |
Caledonite | Pb5Cu2(SO4)3(CO3)(OH)6 | 55.65% | Lanarkite (55.65 %) |
Pyromorphite | Pb5(PO4)3Cl | 55.26% | Ramsbeckite (55.26 %) |
Fluorapatite | Ca5(PO4)3F | 54.54% | Manganohörnesite (54.55 %) |
Löllingite | FeAs2 | 54.54% | Manganohörnesite (54.55 %) |
Ktenasite | ZnCu4(SO4)2(OH)6 · 6H2O | 54.54% | Gordaite (54.55 %) |
Rammelsbergite | NiAs2 | 52.17% | Rösslerite (52.17 %) |
Hydrocerussite | Pb3(CO3)2(OH)2 | 51.30% | Lanarkite (51.30 %) |
Brucite | Mg(OH)2 | 50.57% | Artinite (50.57 %) |
Sideronatrite | Na2Fe(SO4)2(OH) · 3H2O | 50.00% | Ferrinatrite (50.00 %) |
Voltaite | K2Fe2+5Fe3+3Al(SO4)12 · 18H2O | 50.00% | Ferrinatrite (50.00 %) |
Diaphorite | Ag3Pb2Sb3S8 | 50.00% | Ramdohrite (50.00 %) |
Cinnabar | HgS | 43.63% | Rosiaite (54.55 %) |
Safflorite | (Co,Ni,Fe)As2 | 41.73% | Rösslerite (52.17 %) |
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.