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Predictive Mineralogy

Possible unrecorded species at Turquoise ditch (Weinberg Forest), Amstall, Mühldorf, Krems-Land District, Lower Austria, 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%Aragonite (53.70 %), Calcite (62.43 %), Epidote (69.84 %), Fibroferrite (63.93 %), Goethite (66.86 %), Graphite (54.90 %), Halloysite (64.87 %), Huntite (53.95 %), Hydrohalloysite (60.24 %), Jarosite (68.17 %), Magnetite (50.54 %), Muscovite (80.32 %), Nontronite (67.88 %), Nordstrandite (57.69 %), Paragonite (61.36 %), Prehnite (64.07 %), Pyrite (67.27 %), Rutile (72.22 %), Titanite (65.16 %), Todorokite (70.08 %), Tremolite (61.46 %)
Bixbyite-(Mn)Mn3+2O377.27%Ephesite (77.27 %)
ChalcopyriteCuFeS276.21%Jarosite (50.73 %), Pyrite (51.72 %)
HematiteFe2O375.00%Ephesite (50.00 %), Nordstrandite (50.00 %)
GypsumCaSO4 · 2H2O64.75%Fibroferrite (64.75 %)
DiasporeAlO(OH)63.63%Ephesite (63.64 %)
MelanteriteFe2+(H2O)6SO4 · H2O54.91%Fibroferrite (54.92 %)
DolomiteCaMg(CO3)253.94%Huntite (53.95 %)

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
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]

Unique: Halloysite, Nordstrandite
215
48 : Soil leaching zone minerals

Unique: Gibbsite
100
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)19
31 : Thermally altered carbonate, phosphate, and iron formations13
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]13
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)6
6 : Secondary asteroid phases6
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)5
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)5
17 : Marine authigenic Hadean minerals (see also #24)4
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)2
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]2