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Predictive Mineralogy

Possible unrecorded species at Iron Mountain SE[1], Kiowa County, Oklahoma, 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
QuartzSiO297.81%Chalcopyrite (67.26 %), Cuprite (65.19 %), Magnetite (50.54 %), Malachite (61.21 %)
PyriteFeS295.10%Chalcopyrite (75.16 %), Cuprite (58.26 %), Malachite (52.79 %)
CalciteCaCO391.00%Clinohumite (67.38 %), Hydroxylclinohumite (72.41 %)
DiopsideCaMgSi2O684.10%Clinohumite (64.54 %), Hydroxylclinohumite (55.17 %)
ForsteriteMg2SiO480.60%Clinohumite (56.74 %), Hydroxylclinohumite (55.17 %)
AzuriteCu3(CO3)2(OH)251.54%Cuprite (51.54 %)
GalenaPbS40.85%Chalcopyrite (51.07 %)
SphaleriteZnS40.53%Chalcopyrite (50.66 %)

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
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)50
31 : Thermally altered carbonate, phosphate, and iron formations50
35 : Ultra-alkali and agpaitic igneous rocks44
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]44
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]44
53 : Other minerals with taphonomic origins44
54 : Coal and other mine fire minerals (see also #51 and #56)25
50 : Coal and/or oil shale minerals25
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]19
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]19