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Predictive Mineralogy

Possible unrecorded species at Guizhou, China

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
FervaniteFe3+4V5+4O16 · 5H2O100.00%Schubnelite (100.00 %)
BrochantiteCu4(SO4)(OH)698.22%Beaverite-(Cu) (67.66 %), Carbonatecyanotrichite (61.90 %), Cyanotrichite (70.28 %), Otavite (51.61 %)
Taenite(Ni,Fe)98.18%Daubréelite (66.87 %), Native Iron (59.58 %), Schreibersite (69.77 %), Troilite (55.20 %)
HiboniteCaAl12O1985.71%Nierite (85.71 %)
UranophaneCa(UO2)2(SiO3OH)2 · 5H2O82.61%Boltwoodite (50.62 %), Sklodowskite (64.79 %)
Native BismuthBi79.87%Bismite (59.17 %), Parkerite (50.72 %)
TripuhyiteFe3+Sb5+O466.66%Mopungite (66.67 %)
FangiteTl3AsS466.66%Raguinite (66.67 %)
BerylBe3Al2(Si6O18)64.79%Cookeite (60.68 %), Foitite (51.65 %)
BismuthiniteBi2S360.00%Bismite (60.00 %)
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O60.00%Carlhintzeite (60.00 %)
PhosphosideriteFePO4 · 2H2O60.00%Carlhintzeite (60.00 %)
PseudomalachiteCu5(PO4)2(OH)459.29%Libethenite (59.30 %)
Rosasite(Cu,Zn)2(CO3)(OH)258.06%Otavite (58.06 %)
Augite(CaxMgyFez)(Mgy1Fez1)Si2O657.57%Roedderite (57.58 %)
CubaniteCuFe2S356.27%Valleriite (56.27 %)
PyrargyriteAg3SbS355.83%Polybasite (55.84 %)
BrushiteCa(PO3OH) · 2H2O54.54%Sasaite (54.55 %)
MetarossiteCa(V2O6) · 2H2O53.84%Navajoite (53.85 %)
DigeniteCu9S553.45%Idaite (53.46 %)
LinaritePbCu(SO4)(OH)252.09%Beaverite-(Cu) (52.10 %)
CristobaliteSiO251.51%Roedderite (51.52 %)
PharmacoliteCa(HAsO4) · 2H2O50.83%Picropharmacolite (50.83 %)
VrbaiteHg3Tl4As8Sb2S2050.00%Christite (50.00 %)
ElbaiteNa(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH)50.00%Cookeite (50.00 %)
ErythriteCo3(AsO4)2 · 8H2O50.00%Picropharmacolite (50.00 %)
ChalcanthiteCuSO4 · 5H2O50.00%Carlhintzeite (50.00 %)
Rockbridgeite(Fe2+0.5Fe3+0.5)2Fe3+3(PO4)3(OH)550.00%Carlhintzeite (50.00 %)
StrengiteFePO4 · 2H2O50.00%Carlhintzeite (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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Aktashite, Berthierite, Chalcostibite, Clausthalite, Freibergite Subgroup, Galkhaite, etc.
1,865
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Gratonite, Jordisite, Polydymite, Siegenite, Vaesite
498
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Halloysite
362
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Otavite, Smithsonite
280
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Bismite, Wulfenite
274
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hausmannite, Kutnohorite
259
48 : Soil leaching zone minerals

Unique: Gibbsite
130
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Cerianite-(Ce)
106
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
105
1 : Stellar atmosphere condensates

Unique: Nierite
100
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)99
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]80
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]73
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]59
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)58
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]58
34 : Complex granite pegmatites58
53 : Other minerals with taphonomic origins48
6 : Secondary asteroid phases47
4 : Primary chondrule phases45