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Predictive Mineralogy

Possible unrecorded species at Unnamed hot springs, Churata District, Caiza D municipality, Nor Chichas Province, Potosí, Bolivia

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
QuartzSiO294.48%Calcite (62.43 %), Jarosite (68.17 %), Sulphur (53.86 %)
PyriteFeS293.03%Calcite (51.16 %), Jarosite (68.24 %), Sulphur (55.07 %)
GypsumCaSO4 · 2H2O50.28%Sulphur (50.28 %)
ChalcopyriteCuFeS240.58%Jarosite (50.73 %)

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
49 : Oxic cellular biomineralization (see also #44)50
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]49
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]31
46 : Near-surface hydrothermal alteration of minerals (see also #22)31
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]31
44 : Anoxic microbially mediated minerals (see also #44)19
50 : Coal and/or oil shale minerals18
54 : Coal and other mine fire minerals (see also #51 and #56)18
24 : Authigenic minerals in terrestrial sediments (see also #17)18
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)1