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Predictive Mineralogy

Possible unrecorded species at Karadag Reserve (Kara-Dag), Crimea, Ukraine

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
ChalcopyriteCuFeS299.93%Ankerite (62.42 %), Copper (53.15 %), Cuprite (67.05 %), Jarosite (50.73 %), Malachite (60.66 %), Pyrite (51.72 %), Pyrrhotite (76.22 %), Siderite (51.43 %)
SphaleriteZnS63.35%Ankerite (53.36 %), Pyrrhotite (55.40 %)
MagnetiteFe2+Fe3+2O453.48%Augite (53.49 %)
Chabazite-Ca(Ca,K2,Na2)2[Al2Si4O12]2 · 12H2O53.33%Phillipsite-Ca (53.33 %)
BaryteBaSO452.17%Dachiardite-Na (52.17 %)
KaoliniteAl2(Si2O5)(OH)451.68%Alunite (51.69 %)
AzuriteCu3(CO3)2(OH)251.54%Cuprite (51.54 %)
HematiteFe2O350.96%Stilpnomelane (50.96 %)
GalenaPbS43.27%Ankerite (54.09 %)

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
10 : Basalt-hosted zeolite minerals

Unique: Offretite
100
14 : Hot springs, geysers, and other subaerial geothermal minerals9
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)8
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)8
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)8
31 : Thermally altered carbonate, phosphate, and iron formations8
22 : Hydration and low-𝑇 subsurface aqueous alteration (see also #23)7
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]6
9 : Lava/xenolith minerals (hornfels, sanidinite facies)5
35 : Ultra-alkali and agpaitic igneous rocks5
17 : Marine authigenic Hadean minerals (see also #24)4