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Predictive Mineralogy

Possible unrecorded species at Bajna, Komárom-Esztergom County, Hungary

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
QuartzSiO299.94%Baryte (60.21 %), Calcite (62.43 %), Goethite (66.86 %), Jarosite (68.17 %), Marcasite (70.46 %), Pyrite (67.27 %), Rozenite (60.84 %)
ChalcopyriteCuFeS276.58%Jarosite (50.73 %), Marcasite (63.89 %), Pyrite (51.72 %), Rozenite (50.30 %)
SphaleriteZnS52.68%Marcasite (65.85 %)
GalenaPbS46.98%Marcasite (58.73 %)

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
47b : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Sulfates and sulfites]50
45a : Oxidized fumarolic minerals (see also [#11]) - [Sulfates, arsenates, selenates, antimonates]50
50 : Coal and/or oil shale minerals38
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]33
49 : Oxic cellular biomineralization (see also #44)30
54 : Coal and other mine fire minerals (see also #51 and #56)28
55 : Anthropogenic mine minerals22
21 : Chemically precipitated carbonate, phosphate, iron formations21
46 : Near-surface hydrothermal alteration of minerals (see also #22)19
25 : Evaporites (prebiotic)14