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Predictive Mineralogy

Possible unrecorded species at Nagypisznice Quarry, Lábatlan, 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
QuartzSiO299.87%Aragonite (53.70 %), Baryte (60.21 %), Calcite (62.43 %), Goethite (66.86 %), Hematite (62.61 %), Manganite (51.54 %), Marcasite (70.46 %)
PyriteFeS299.28%Baryte (50.79 %), Calcite (51.16 %), Goethite (55.41 %), Hematite (50.17 %), Marcasite (86.56 %)
PyrolusiteMn4+O263.98%Manganite (63.98 %)
SphaleriteZnS52.68%Marcasite (65.85 %)
ChalcopyriteCuFeS251.11%Marcasite (63.89 %)
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
14 : Hot springs, geysers, and other subaerial geothermal minerals50
49 : Oxic cellular biomineralization (see also #44)39
24 : Authigenic minerals in terrestrial sediments (see also #17)36
48 : Soil leaching zone minerals35
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]35
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]34
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)29
53 : Other minerals with taphonomic origins26
55 : Anthropogenic mine minerals24
17 : Marine authigenic Hadean minerals (see also #24)21