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Predictive Mineralogy

Possible unrecorded species at Hautes-Pyrénées, 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
SilverAg99.17%Breithauptite (50.99 %), Dyscrasite (58.82 %), Pararammelsbergite (50.85 %), Pearceite (58.12 %), Safflorite (59.63 %), Skutterudite (50.92 %)
Goethiteα-Fe3+O(OH)96.50%Cesàrolite (69.44 %), Devilline (51.87 %), Langite (50.97 %), Serpierite (51.59 %)
CupriteCu2O95.82%Cesàrolite (50.00 %), Devilline (53.50 %), Langite (59.73 %), Serpierite (55.36 %)
JacobsiteMn2+Fe3+2O487.69%Sarkinite (50.00 %), Sonolite (50.79 %), Sussexite (50.00 %)
BerylBe3Al2(Si6O18)87.59%Columbite-(Fe) (57.46 %), Columbite-(Mn) (70.83 %)
Neotocite(Mn,Fe,Mg)SiO3 · H2O75.00%Sarkinite (50.00 %), Welinite (50.00 %)
AcanthiteAg2S63.96%Pearceite (63.96 %)
PhlogopiteKMg3(AlSi3O10)(OH)259.00%Humite (59.00 %)
AegirineNaFe3+Si2O657.57%Baotite (57.58 %)
SmithsoniteZnCO355.58%Hemimorphite (55.59 %)
Piemontite-(Sr)(CaSr)(AlAlMn3+)O[Si2O7][SiO4](OH)55.55%Epidote-(Sr) (55.56 %)
MimetitePb5(AsO4)3Cl55.55%Cesàrolite (55.56 %)
CarnotiteK2(UO2)2(VO4)2 · 3H2O54.81%Tyuyamunite (54.81 %)
ChalcanthiteCuSO4 · 5H2O53.33%Moorhouseite (53.33 %)
PyromorphitePb5(PO4)3Cl52.77%Cesàrolite (52.78 %)
Polybasite[Ag6Sb2S7][Ag9CuS4]51.29%Pearceite (51.30 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
PyrochroiteMn(OH)250.00%Welinite (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.

Paragenetic ModeScore
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Argutite, Friedelite, Hausmannite, Kutnohorite, Parsettensite, Pyrosmalite-(Fe), etc.
987
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Dyscrasite, Glaucodot, Melanostibite, Pararammelsbergite, Pearceite, Rammelsbergite, etc.
841
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)

Unique: Vuorelainenite
176
34 : Complex granite pegmatites

Unique: Ishikawaite
168
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Sussexite
147
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Brunogeierite
118
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Siegenite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]96
26 : Hadean detrital minerals54
31 : Thermally altered carbonate, phosphate, and iron formations44
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]39
36 : Carbonatites, kimberlites, and related igneous rocks37
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)36
35 : Ultra-alkali and agpaitic igneous rocks36
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]26
37 : Layered igneous intrusions and related PGE minerals26
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]25