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Predictive Mineralogy

Possible unrecorded species at Mendoza Province, Argentina

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
HaliteNaCl99.63%Bl枚dite (67.11 %), Kieserite (63.44 %), Sylvite (81.54 %), Syngenite (62.75 %), Th茅nardite (56.29 %)
HessiteAg2Te97.51%Cervelleite (67.86 %), St眉tzite (84.00 %), Tellurobismuthite (51.61 %)
TorberniteCu(UO2)2(PO4)2 路 12H2O97.27%Dewindtite (63.04 %), Johannite (56.25 %), Sengierite (64.71 %), Uranopilite (52.21 %)
MetarossiteCa(V2O6) 路 2H2O77.77%Rossite (77.78 %)
AltaitePbTe65.59%St眉tzite (65.60 %)
PascoiteCa2Ca(V10O28) 路 17H2O63.88%Rossite (63.89 %)
PetziteAg3AuTe262.40%St眉tzite (62.40 %)
RhodochrositeMnCO357.74%Neotocite (57.75 %)
AnalcimeNa(AlSi2O6) 路 H2O57.41%Thomsonite-Ca (57.41 %)
AnhydriteCaSO454.83%Kieserite (54.84 %)
MetatorberniteCu(UO2)2(PO4)2 路 8H2O52.94%Sengierite (52.94 %)
SylvaniteAgAuTe451.20%St眉tzite (51.20 %)
MicroclineK(AlSi3O8)50.00%Potassic-hastingsite (50.00 %)
TiemanniteHgSe43.63%Trogtalite (54.55 %)

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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Ach谩valite, Bornhardtite, Boulangerite, Cervelleite, Clausthalite, Cosalite, etc.
2,106
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Cuprotungstite
187
47g : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite, Iodargyrite
172
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
117
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Potassic-ferro-ferri-sadanagaite
108
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Gratonite
100
53 : Other minerals with taphonomic origins44
47f : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U鈦垛伜) minerals]43
49 : Oxic cellular biomineralization (see also #44)41
31 : Thermally altered carbonate, phosphate, and iron formations41
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]34
52 : Guano- and urine-derived minerals29
6 : Secondary asteroid phases27
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)27
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]24
47e : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]24