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Predictive Mineralogy

Possible unrecorded species at Sennigrat-Kreuzjoch-Hochjoch area, Schruns, Bludenz District, Vorarlberg, Austria

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
QuartzSiO299.99%Albite (78.81 %), Chabazite-Ca (50.66 %), Chalcopyrite (67.26 %), Chamosite (79.57 %), Epidote (69.84 %), Hematite (62.61 %), Heulandite-Ca (66.33 %), Jarosite (68.17 %), Kyanite (53.58 %), Malachite (61.21 %), Microcline (81.52 %), Muscovite (80.32 %), Orthoclase (76.14 %), Prehnite (64.07 %), Pyrite (67.27 %), Rutile (72.22 %), Stellerite (63.21 %), Stilbite-Ca (66.16 %), Titanite (65.16 %)
CalciteCaCO399.97%Chabazite-Ca (72.56 %), Chamosite (60.72 %), Epidote (51.60 %), Heulandite-Ca (66.67 %), Jarosite (50.12 %), Prehnite (61.24 %), Stellerite (62.26 %), Stilbite-Ca (65.55 %), Titanite (52.17 %)
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
10 : Basalt-hosted zeolite minerals

Unique: Stellerite
100
24 : Authigenic minerals in terrestrial sediments (see also #17)5
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]5
31 : Thermally altered carbonate, phosphate, and iron formations4
53 : Other minerals with taphonomic origins4
6 : Secondary asteroid phases4
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]4
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)3
26 : Hadean detrital minerals3
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)2
36 : Carbonatites, kimberlites, and related igneous rocks2