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Predictive Mineralogy

Possible unrecorded species at Mád, 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
CalciteCaCO395.42%Bariopharmacosiderite (52.15 %), Baryte (51.88 %), Montmorillonite (52.16 %), Mordenite (58.45 %)
ArsenopyriteFeAsS89.31%Pharmacosiderite (58.74 %), Scorodite (74.10 %)
ChalcopyriteCuFeS278.90%Bariopharmacosiderite (67.20 %), Dickite (54.00 %), Pharmacosiderite (59.35 %), Pyrite (51.72 %), Scorodite (53.74 %)
GalenaPbS75.50%Bariopharmacosiderite (53.23 %), Dickite (50.00 %), Pharmacosiderite (51.63 %), Scorodite (50.30 %)
MalachiteCu2(CO3)(OH)252.04%Bariopharmacosiderite (65.05 %)
AzuriteCu3(CO3)2(OH)243.44%Bariopharmacosiderite (54.30 %)
BrochantiteCu4(SO4)(OH)641.29%Bariopharmacosiderite (51.61 %)
OliveniteCu2(AsO4)(OH)40.86%Bariopharmacosiderite (51.08 %)

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]50
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]41
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)14
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)9
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)6
55 : Anthropogenic mine minerals5
28 : Photo-alteration, pre-biotic5
24 : Authigenic minerals in terrestrial sediments (see also #17)2
6 : Secondary asteroid phases2
53 : Other minerals with taphonomic origins2