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Predictive Mineralogy

Possible unrecorded species at Matanuska-Susitna Borough, Alaska, 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
PetziteAg3AuTe278.61%Coloradoite (54.85 %), Nagyágite (52.63 %)
BerylBe3Al2(Si6O18)74.68%Wodginite (74.68 %)
AlbiteNa(AlSi3O8)73.41%Wodginite (73.42 %)
MicroclineK(AlSi3O8)62.02%Wodginite (62.03 %)
SperrylitePtAs252.32%Isoferroplatinum (52.33 %)
ScoroditeFe3+AsO4 · 2H2O50.66%Pitticite (50.67 %)
Osmium(Os,Ir,Ru)45.88%Iridium (57.36 %)
LauriteRuS244.18%Isoferroplatinum (55.23 %)
SpodumeneLiAlSi2O640.50%Wodginite (50.63 %)

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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Coloradoite, Hessite, Miargyrite, Nagyágite, Pyrargyrite
487
34 : Complex granite pegmatites

Unique: Wodginite
100
6 : Secondary asteroid phases18
26 : Hadean detrital minerals16
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]15
36 : Carbonatites, kimberlites, and related igneous rocks13
49 : Oxic cellular biomineralization (see also #44)12
37 : Layered igneous intrusions and related PGE minerals10
53 : Other minerals with taphonomic origins10
38 : Ophiolites9
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]8
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)7