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URL: https://www.mindat.org/missing_minerals.php?id=224043

⇱ Predictive Mineralogy

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Predictive Mineralogy

Possible unrecorded species at Ting Creek intrusion, Watson Lake mining district, Yukon, 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
PyriteFeS299.99%Arsenopyrite (79.40 %), Epidote (56.37 %), Galena (66.84 %), Hematite (50.17 %), Molybdenite (68.29 %), Pyrrhotite (80.12 %), Sphalerite (75.10 %), Stibnite (62.99 %)
CalciteCaCO399.71%Analcime (57.00 %), Cancrinite (61.52 %), Chondrodite (65.81 %), Epidote (51.60 %), Hastingsite (50.17 %), Phlogopite (55.90 %), Titanite (52.17 %)
MuscoviteKAl2(AlSi3O10)(OH)281.82%Albite (52.80 %), Microcline (61.50 %)
ChalcopyriteCuFeS279.54%Arsenopyrite (61.33 %), Galena (56.79 %), Molybdenite (60.83 %), Pyrrhotite (76.22 %), Sphalerite (63.80 %)
NatroliteNa2Al2Si3O10 · 2H2O54.68%Mosandrite-(Ce) (54.69 %)
DiopsideCaMgSi2O654.63%Chondrodite (54.63 %)

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
35 : Ultra-alkali and agpaitic igneous rocks

Unique: Astrophyllite, Låvenite, Mosandrite-(Ce)		100
31 : Thermally altered carbonate, phosphate, and iron formations2
36 : Carbonatites, kimberlites, and related igneous rocks2
9 : Lava/xenolith minerals (hornfels, sanidinite facies)2
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)1
17 : Marine authigenic Hadean minerals (see also #24)1
19 : Granitic intrusive rocks1
34 : Complex granite pegmatites1
37 : Layered igneous intrusions and related PGE minerals1
50 : Coal and/or oil shale minerals1
54 : Coal and other mine fire minerals (see also #51 and #56)1