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Predictive Mineralogy

Possible unrecorded species at Coume de Ponteils, Sansa, Prades, Pyrénées-Orientales, Occitanie, France

This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.

Possible missing speciesFormulaMatch %Due to recorded presence of
QuartzSiO291.07%Diopside (51.68 %), Microcline (81.52 %)
MuscoviteKAl2(AlSi3O10)(OH)261.50%Microcline (61.50 %)
AlbiteNa(AlSi3O8)56.11%Microcline (56.11 %)
CalciteCaCO354.06%Diopside (54.07 %)

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.

Paragenetic ModeScore
35 : Ultra-alkali and agpaitic igneous rocks50
34 : Complex granite pegmatites46
26 : Hadean detrital minerals46
24 : Authigenic minerals in terrestrial sediments (see also #17)46
19 : Granitic intrusive rocks46
54 : Coal and other mine fire minerals (see also #51 and #56)4
50 : Coal and/or oil shale minerals4
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)4
38 : Ophiolites4
37 : Layered igneous intrusions and related PGE minerals4