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Predictive Mineralogy

Possible unrecorded species at Pegmatite No. 10, Buck claim, Bernic Lake, Lac-du-Bonnet area, Manitoba, Canada

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
MuscoviteKAl2(AlSi3O10)(OH)298.82%Amblygonite (69.57 %), Beryl (55.56 %), Spodumene (62.28 %), Triphylite (76.88 %)
AlbiteNa(AlSi3O8)96.37%Amblygonite (69.20 %), Spodumene (62.28 %), Triphylite (68.79 %)
MicroclineK(AlSi3O8)55.49%Triphylite (55.49 %)
SchorlNaFe2+3Al6(Si6O18)(BO3)3(OH)3(OH)42.08%Triphylite (52.60 %)

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
34 : Complex granite pegmatites

Unique: Spodumene, Triphylite
100
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]2
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]2
35 : Ultra-alkali and agpaitic igneous rocks0
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)0
19 : Granitic intrusive rocks0
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)0
20 : Acidic volcanic rocks0
10 : Basalt-hosted zeolite minerals0
5 : Primary asteroid phases0
6 : Secondary asteroid phases0