Predictive Mineralogy
Possible unrecorded species at Hashupa epidote occurrence, Hashupa alpine-type clefts, Hashupa, Shigar Valley, Shigar District, Gilgit-Baltistan, Pakistan
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 |
---|---|---|---|
Pyrite | FeS2 | 99.92% | Actinolite (62.14 %), Baryte (50.79 %), Calcite (51.16 %), Clinochlore (51.79 %), Clinozoisite (51.74 %), Epidote (56.37 %), Hematite (50.17 %), Rutile (52.79 %), Siderite (66.11 %) |
Muscovite | KAl2(AlSi3O10)(OH)2 | 61.50% | Microcline (61.50 %) |
Chalcopyrite | CuFeS2 | 61.44% | Actinolite (52.26 %), Siderite (51.43 %) |
Albite | Na(AlSi3O8) | 56.11% | Microcline (56.11 %) |
Magnetite | Fe2+Fe3+2O4 | 53.37% | Actinolite (53.38 %) |
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.