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Predictive Mineralogy

Possible unrecorded species at Quarry by the railway, Rátka, Szerencs District, Borsod-Abaúj-Zemplén 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
PyriteFeS297.01%Goethite (55.41 %), Hematite (50.17 %), Marcasite (86.56 %)
CalciteCaCO395.44%Clinoptilolite-Ca (72.09 %), Marcasite (60.67 %), Mordenite (58.45 %)
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
24 : Authigenic minerals in terrestrial sediments (see also #17)50
10 : Basalt-hosted zeolite minerals47
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)45
48 : Soil leaching zone minerals38
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)36
14 : Hot springs, geysers, and other subaerial geothermal minerals22
9 : Lava/xenolith minerals (hornfels, sanidinite facies)19
25 : Evaporites (prebiotic)18
49 : Oxic cellular biomineralization (see also #44)15
17 : Marine authigenic Hadean minerals (see also #24)14