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Predictive Mineralogy

Possible unrecorded species at Sierra Almagrera, Cuevas del Almanzora, AlmerĂ­a, Andalusia, Spain

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
CupriteCu2O99.93%Chalcoalumite (66.67 %), Connellite (72.41 %), Cumengeite (55.36 %), Cyanotrichite (53.77 %), Fougèrite (52.17 %), Gartrellite (57.14 %), Schulenbergite (64.15 %), Serpierite (55.36 %)
AragoniteCaCO397.66%Brianyoungite (52.69 %), Fougèrite (73.91 %), Laurionite (55.17 %), Schulenbergite (57.86 %)
OliveniteCu2(AsO4)(OH)97.48%Arsentsumebite (58.54 %), Bayldonite (52.26 %), Gartrellite (71.43 %), Natropharmacosiderite (55.56 %)
CopperCu96.21%Chalcoalumite (58.10 %), Connellite (59.48 %), Fougèrite (52.17 %), Laurionite (53.45 %)
StibniteSb2S395.85%Semseyite (53.77 %), Valentinite (78.50 %), Veenite (58.33 %)
MuscoviteKAl2(AlSi3O10)(OH)289.50%Albite (52.80 %), Dravite (55.53 %), Veenite (50.00 %)
HemimorphiteZn4Si2O7(OH)2 · H2O88.64%Arsentsumebite (53.66 %), Brianyoungite (50.54 %), Hetaerolite (50.46 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 185.11%Arsentsumebite (68.29 %), Gartrellite (53.06 %)
LangiteCu4(SO4)(OH)6 · 2H2O84.49%Fougèrite (60.87 %), Schulenbergite (60.38 %)
HydrozinciteZn5(CO3)2(OH)683.43%Brianyoungite (62.37 %), Schulenbergite (55.97 %)
DuftitePbCu(AsO4)(OH)82.08%Arsentsumebite (56.10 %), Gartrellite (59.18 %)
FluoriteCaF280.00%Zharchikhite (80.00 %)
PyromorphitePb5(PO4)3Cl79.08%Gartrellite (53.06 %), Plumbogummite (55.45 %)
HydrocerussitePb3(CO3)2(OH)276.91%Fougèrite (52.17 %), Laurionite (51.72 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)676.66%Brianyoungite (50.54 %), Schulenbergite (52.83 %)
KaoliniteAl2(Si2O5)(OH)476.47%Alunite (51.69 %), Natroalunite (51.30 %)
RutileTiO256.67%Brookite (56.67 %)
LeadPb56.52%Fougèrite (56.52 %)
LavendulanNaCaCu5(AsO4)4Cl · 5H2O55.55%Natropharmacosiderite (55.56 %)
DolomiteCaMg(CO3)252.68%Brianyoungite (52.69 %)
LithargePbO52.17%Fougèrite (52.17 %)
ParalaurionitePbCl(OH)51.72%Laurionite (51.72 %)
AdamiteZn2(AsO4)(OH)51.02%Gartrellite (51.02 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
AcanthiteAg2S50.00%Veenite (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: Boulangerite, Bournonite, Semseyite, Veenite
424
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]162
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
147
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]134
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite
119
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits

Unique: Hetaerolite
100
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]63
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]30
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)16
56 : Slag and smelter minerals (see also #51 and #55)16
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)15
37 : Layered igneous intrusions and related PGE minerals13
10 : Basalt-hosted zeolite minerals12
55 : Anthropogenic mine minerals10