Predictive Mineralogy
Possible unrecorded species at Khurayyim Mount (Jabal al Khurayyim), Daba-Siwaqa complex, Transjordan Plateau, Amman Governorate, Jordan
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 | 99.98% | Calcite (62.43 %), Chalcocite (63.99 %), Clinohedrite (66.67 %), Fluorapatite (70.90 %), Franklinite (51.52 %), Hematite (62.61 %), Pyrite (67.27 %), Sphalerite (67.53 %), Thaumasite (51.69 %) |
| Chalcopyrite | CuFeS2 | 98.52% | Chalcocite (74.77 %), Clinohedrite (66.67 %), Pyrite (51.72 %), Sphalerite (63.80 %) |
| Magnetite | Fe2+Fe3+2O4 | 98.43% | Clinohedrite (55.56 %), Cuspidine (56.47 %), Franklinite (56.06 %), Magnesioferrite (59.50 %), Thaumasite (54.59 %) |
| Wollastonite | Ca3(Si3O9) | 98.39% | Cuspidine (67.06 %), Foshagite (72.00 %), Jennite (54.17 %), Spurrite (61.97 %) |
| Andradite | Ca3Fe3+2(SiO4)3 | 92.15% | Clinohedrite (66.67 %), Cuspidine (52.94 %), Jennite (50.00 %) |
| Katoite | Ca3Al2[◻(OH)4]3 | 91.42% | Fluorkyuygenite (80.00 %), Fluormayenite (57.14 %) |
| Diopside | CaMgSi2O6 | 83.48% | Cuspidine (54.12 %), Foshagite (64.00 %) |
| Gypsum | CaSO4 · 2H2O | 81.34% | Clinohedrite (55.56 %), Ettringite (58.04 %) |
| Brownmillerite | Ca2(Al,Fe3+)2O5 | 71.42% | Fluormayenite (71.43 %) |
| Fluorellestadite | Ca5(SiO4)1.5(SO4)1.5F | 71.42% | Fluormayenite (71.43 %) |
| Periclase | MgO | 71.42% | Fluormayenite (71.43 %) |
| Galena | PbS | 70.79% | Franklinite (54.55 %), Sphalerite (74.68 %) |
| Dolomite | CaMg(CO3)2 | 66.66% | Clinohedrite (66.67 %) |
| Muscovite | KAl2(AlSi3O10)(OH)2 | 66.66% | Clinohedrite (66.67 %) |
| Hydrocalumite | Ca4Al2(OH)12(Cl,CO3,OH)2 · 4H2O | 64.28% | Fluormayenite (57.14 %), Jennite (54.17 %) |
| Vesuvianite | Ca19Fe3+Al4(Al6Mg2)(◻4)◻[Si2O7]4[(SiO4)10]O(OH)9 | 64.00% | Foshagite (64.00 %) |
| Tobermorite | Ca4Si6O17(H2O)2 · (Ca · 3H2O) | 62.50% | Jennite (62.50 %) |
| Perovskite | CaTiO3 | 60.70% | Cuspidine (51.76 %), Jennite (50.00 %) |
| Afwillite | Ca3(HSiO4)2 · 2H2O | 58.33% | Jennite (58.33 %) |
| Larnite | Ca2SiO4 | 57.14% | Fluormayenite (57.14 %) |
| Portlandite | Ca(OH)2 | 57.14% | Fluormayenite (57.14 %) |
| Nabimusaite | KCa12(SiO4)4(SO4)2O2F | 57.14% | Fluormayenite (57.14 %) |
| Malachite | Cu2(CO3)(OH)2 | 56.19% | Chalcocite (56.20 %) |
| Copper | Cu | 55.55% | Clinohedrite (55.56 %) |
| Goethite | α-Fe3+O(OH) | 55.55% | Clinohedrite (55.56 %) |
| Willemite | Zn2SiO4 | 55.55% | Clinohedrite (55.56 %) |
| Xonotlite | Ca6(Si6O17)(OH)2 | 55.55% | Clinohedrite (55.56 %) |
| Aragonite | CaCO3 | 54.46% | Ettringite (54.46 %) |
| Baryte | BaSO4 | 53.33% | Clinohedrite (66.67 %) |
| Grossular | Ca3Al2(SiO4)3 | 52.00% | Foshagite (52.00 %) |
| Vorlanite | Ca(U6+)O4 | 45.71% | Fluormayenite (57.14 %) |
| Vapnikite | Ca2CaUO6 | 45.71% | Fluormayenite (57.14 %) |
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.