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Predictive Mineralogy

Possible unrecorded species at Chloride Flat Mining District [includes Silver City Mining District], Grant County, New Mexico, USA

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
VivianiteFe2+Fe2+2(PO4)2 · 8H2O82.66%Ludlamite (82.67 %)
FluorapatiteCa5(PO4)3F68.00%Ludlamite (68.00 %)
BrochantiteCu4(SO4)(OH)667.66%Beaverite-(Cu) (67.66 %)
AzuriteCu3(CO3)2(OH)265.26%Beaverite-(Cu) (65.27 %)
ArsenopyriteFeAsS58.66%Ludlamite (58.67 %)
DiopsideCaMgSi2O652.26%Grossular (52.27 %)
LinaritePbCu(SO4)(OH)252.09%Beaverite-(Cu) (52.10 %)
AutuniteCa(UO2)2(PO4)2 · 10-12H2O51.51%Torbernite (51.52 %)
TriphyliteLiFe2+PO444.80%Ludlamite (56.00 %)
Polybasite[Ag6Sb2S7][Ag9CuS4]41.03%Pearceite (51.30 %)
BerylBe3Al2(Si6O18)40.53%Ludlamite (50.67 %)

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
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]

Unique: Bromargyrite, Chlorargyrite, Iodargyrite
275
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Pearceite
104
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]38
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]30
50 : Coal and/or oil shale minerals14
54 : Coal and other mine fire minerals (see also #51 and #56)14
49 : Oxic cellular biomineralization (see also #44)14
34 : Complex granite pegmatites13
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)12
53 : Other minerals with taphonomic origins6
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]5
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]4