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Predictive Mineralogy

Possible unrecorded species at San José claim (Los Sejas mine; El Negre mine), Chóvar, Castellón, Valencian Community, 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
PyriteFeS299.99%Adamite (59.33 %), Asbolane (54.76 %), Atacamite (50.08 %), Azurite (58.39 %), Baryte (50.79 %), Bieberite (71.43 %), Chalcanthite (74.95 %), Clinoclase (50.68 %), Fletcherite (62.50 %), Hematite (50.17 %), Jarosite (68.24 %), Libethenite (56.49 %), Malachite (52.79 %), Marcasite (86.56 %), Metazeunerite (58.33 %), Olivenite (56.33 %), Pharmacosiderite (64.43 %), Pseudomalachite (52.35 %), Zeunerite (58.14 %)
ChalcopyriteCuFeS299.99%Adamite (60.33 %), Asbolane (52.38 %), Atacamite (53.76 %), Azurite (65.18 %), Bieberite (60.71 %), Chalcanthite (74.56 %), Clinoclase (65.07 %), Fletcherite (68.75 %), Jarosite (50.73 %), Libethenite (61.75 %), Malachite (60.66 %), Marcasite (63.89 %), Metazeunerite (59.72 %), Olivenite (65.16 %), Pharmacosiderite (59.35 %), Pseudomalachite (63.85 %), Zeunerite (59.07 %)
CalciteCaCO399.81%Adamite (67.67 %), Asbolane (50.00 %), Baryte (51.88 %), Bieberite (50.00 %), Chalcanthite (50.00 %), Jarosite (50.12 %), Marcasite (60.67 %), Olivenite (50.43 %)
SphaleriteZnS96.74%Adamite (55.00 %), Bieberite (53.57 %), Chalcanthite (54.35 %), Marcasite (65.85 %)
GalenaPbS79.69%Adamite (66.33 %), Bieberite (50.00 %), Chalcanthite (53.97 %), Fletcherite (50.00 %), Marcasite (58.73 %), Olivenite (50.95 %), Pharmacosiderite (51.63 %)
CupriteCu2O77.63%Clinoclase (54.79 %), Libethenite (50.53 %)
UraniniteUO276.95%Metazeunerite (53.70 %), Zeunerite (50.23 %)
ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 176.70%Clinoclase (52.74 %), Pseudomalachite (50.70 %)
ChalcociteCu2S62.50%Fletcherite (62.50 %)
CovelliteCuS62.50%Fletcherite (62.50 %)
ScoroditeFe3+AsO4 · 2H2O61.99%Pharmacosiderite (61.99 %)
ArsenopyriteFeAsS58.73%Pharmacosiderite (58.74 %)
CornwalliteCu5(AsO4)2(OH)458.21%Clinoclase (58.22 %)
BorniteCu5FeS456.25%Fletcherite (56.25 %)
BrochantiteCu4(SO4)(OH)655.47%Clinoclase (55.48 %)
GypsumCaSO4 · 2H2O55.35%Bieberite (55.36 %)
SiegeniteCoNi2S450.00%Fletcherite (50.00 %)
CerussitePbCO348.00%Adamite (60.00 %)
MimetitePb5(AsO4)3Cl46.93%Adamite (58.67 %)

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: Fletcherite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]96
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]48
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]32
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]14
53 : Other minerals with taphonomic origins8
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]7
56 : Slag and smelter minerals (see also #51 and #55)4
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]2
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)2
42 : Sea-floor Mn nodules2