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Predictive Mineralogy

Possible unrecorded species at Bourgogne-Franche-Comt茅, 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
LanarkitePb2(SO4)O91.66%Macphersonite (75.00 %), Scotlandite (66.67 %)
MottramitePbCu(VO4)(OH)87.30%Plumbotsumite (71.43 %), Scotlandite (55.56 %)
DioptaseCuSiO3 路 H2O85.71%Plumbotsumite (85.71 %)
LazuliteMgAl2(PO4)2(OH)280.00%Trolleite (80.00 %)
MetazeuneriteCu(UO2)2(AsO4)2 路 8H2O75.00%Arsenuranospathite (75.00 %)
AugeliteAl2(PO4)(OH)375.00%Trolleite (75.00 %)
ChlorargyriteAgCl71.42%Plumbotsumite (71.43 %)
FornacitePb2Cu(CrO4)(AsO4)(OH)71.42%Plumbotsumite (71.43 %)
CornubiteCu5(AsO4)2(OH)466.66%Bariopharmacoalumite (66.67 %)
CornwalliteCu5(AsO4)2(OH)466.66%Bariopharmacoalumite (66.67 %)
Schoepite(UO2)8O2(OH)12 路 12H2O65.71%Ianthinite (65.71 %)
UranospiniteCa(UO2)2(AsO4)2 路 10H2O62.50%Arsenuranospathite (62.50 %)
PetziteAg3AuTe262.40%St眉tzite (62.40 %)
KyaniteAl2(SiO4)O60.00%Trolleite (60.00 %)
MattheddleitePb5(SiO4)1.5(SO4)1.5(Cl,OH)59.25%Scotlandite (59.26 %)
BayldonitePbCu3(AsO4)2(OH)258.82%Arsenogorceixite (58.82 %)
ChalcophylliteCu18Al2(AsO4)4(SO4)3(OH)24 路 36H2O58.33%Bariopharmacoalumite (58.33 %)
SkutteruditeCoAs358.28%Safflorite (58.29 %)
AtacamiteCu2(OH)3Cl57.14%Plumbotsumite (57.14 %)
BoleiteKPb26Ag9Cu24(OH)48Cl6257.14%Plumbotsumite (57.14 %)
CreaseyitePb2Cu2Fe3+2(Si4.67Al0.33)O15.33(OH)3 路 H2O57.14%Plumbotsumite (57.14 %)
PlattneritePbO257.14%Plumbotsumite (57.14 %)
PhosphohedyphaneCa2Pb3(PO4)3Cl57.14%Plumbotsumite (57.14 %)
FluorapatiteCa5(PO4)3F56.33%Scorzalite (56.34 %)
ConichalciteCaCu(AsO4)(OH)52.17%Arsenogoyazite (52.17 %)
SylvaniteAgAuTe451.20%St眉tzite (51.20 %)
NatrozippeiteNa5(UO2)8(SO4)4O5(OH)3 路 12H2O50.00%Magnesiozippeite (50.00 %)
MassicotPbO50.00%Macphersonite (50.00 %)
AdamiteZn2(AsO4)(OH)50.00%Zincolivenite (50.00 %)
Rutherfordine(UO2)CO350.00%Arsenuranospathite (50.00 %)
LavendulanNaCaCu5(AsO4)4Cl 路 5H2O50.00%Bariopharmacoalumite (50.00 %)
BerliniteAlPO450.00%Trolleite (50.00 %)
IodargyriteAgI45.71%Plumbotsumite (57.14 %)
MunakataitePb2Cu2(Se4+O3)(SO4)(OH)445.71%Plumbotsumite (57.14 %)

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: Aikinite, Arsenic, Betekhtinite, Bournonite, Colusite, Cosalite, etc.
2,120
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Ferrimolybdite, Hydrotungstite, Hydroxykenoelsmoreite, Markascherite, Tungstite
915
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Raspite, Stolzite, Wulfenite
345
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Bixbyite-(Mn), Hausmannite, Kutnohorite
308
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
243
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]207
47f : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U鈦垛伜) minerals]117
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: K毛sterite
109
52 : Guano- and urine-derived minerals

Unique: Nitromagnesite
100
47b : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]85
34 : Complex granite pegmatites66
26 : Hadean detrital minerals46
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)45
6 : Secondary asteroid phases39
53 : Other minerals with taphonomic origins38
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)38
35 : Ultra-alkali and agpaitic igneous rocks30