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Predictive Mineralogy

Possible unrecorded species at Santa Rosa-Huantajaya mining district, Iquique Province, Tarapacá, Chile

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
CerussitePbCO399.75%Boleite (59.76 %), Marshite (68.75 %), Herbertsmithite (52.00 %), Mimetite (66.77 %), Pseudoboleite (70.73 %), Wulfenite (58.77 %)
AnglesitePbSO495.82%Boleite (58.54 %), Marshite (62.50 %), Pseudoboleite (73.17 %)
BorniteCu5FeS475.95%Marshite (50.00 %), Stromeyerite (51.92 %)
CupriteCu2O68.75%Marshite (68.75 %)
CopperCu68.75%Marshite (68.75 %)
PhosgenitePb2CO3Cl263.41%Pseudoboleite (63.41 %)
BrochantiteCu4(SO4)(OH)656.25%Marshite (56.25 %)
Goethiteα-Fe3+O(OH)56.25%Marshite (56.25 %)
DiaboleitePb2CuCl2(OH)456.09%Pseudoboleite (56.10 %)
MuscoviteKAl2(AlSi3O10)(OH)252.79%Albite (52.80 %)
HemimorphiteZn4Si2O7(OH)2 · H2O52.00%Herbertsmithite (52.00 %)
IodargyriteAgI50.00%Marshite (50.00 %)
MolybdeniteMoS250.00%Marshite (50.00 %)
BaryteBaSO442.36%Tyrolite (52.96 %)
GoldAu40.00%Marshite (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
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Chlorargyrite, Marshite
196
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Juangodoyite, Sanrománite
179
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Enargite, Stromeyerite
170
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]50
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]12
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]11
25 : Evaporites (prebiotic)11
49 : Oxic cellular biomineralization (see also #44)11
53 : Other minerals with taphonomic origins7
56 : Slag and smelter minerals (see also #51 and #55)6
50 : Coal and/or oil shale minerals4
57 : Other minerals formed by human processes3
36 : Carbonatites, kimberlites, and related igneous rocks2