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Predictive Mineralogy

Possible unrecorded species at Cadafaz e Colmeal, Góis, Coimbra, Portugal

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
BerauniteFe3+6(PO4)4O(OH)4 · 6H2O83.33%Plimerite (83.33 %)
GalenaPbS79.81%Arsenopyrite (53.61 %), Chalcopyrite (51.07 %), Covellite (64.18 %), Pharmacosiderite (51.63 %), Scorodite (50.30 %), Silver (52.62 %), Sphalerite (74.68 %)
GypsumCaSO4 · 2H2O66.66%Plimerite (66.67 %)
RockbridgeiteFe2+Fe3+4(PO4)3(OH)566.66%Plimerite (66.67 %)
CalciteCaCO355.86%Lepidocrocite (55.87 %)
HematiteFe2O355.12%Lepidocrocite (55.13 %)
MalachiteCu2(CO3)(OH)254.65%Covellite (54.66 %)
ChalcociteCu2S50.30%Covellite (50.30 %)
DufréniteCa0.5Fe2+Fe3+5(PO4)4(OH)6 · 2H2O50.00%Plimerite (50.00 %)
FluorapatiteCa5(PO4)3F50.00%Plimerite (50.00 %)
JarositeKFe3+3(SO4)2(OH)650.00%Plimerite (50.00 %)
MuscoviteKAl2(AlSi3O10)(OH)250.00%Plimerite (50.00 %)
TorberniteCu(UO2)2(PO4)2 · 12H2O40.00%Plimerite (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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]50
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]26
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]24
55 : Anthropogenic mine minerals7
21 : Chemically precipitated carbonate, phosphate, iron formations4
38 : Ophiolites3
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])3
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)2
26 : Hadean detrital minerals2
36 : Carbonatites, kimberlites, and related igneous rocks2