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Predictive Mineralogy

Possible unrecorded species at Tyuya-Muyun Cu-V-U deposit, Tyuya-Muyun Massif, Aravan District, Osh Region, Kyrgyzstan

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
CerussitePbCO392.05%Descloizite (60.18 %), Mottramite (56.64 %), Vanadinite (54.01 %)
ScoroditeFe3+AsO4 · 2H2O57.52%Arseniosiderite (57.52 %)
AzuriteCu3(CO3)2(OH)256.70%Conichalcite (56.71 %)
WulfenitePb(MoO4)40.11%Vanadinite (50.14 %)

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
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]34
53 : Other minerals with taphonomic origins16
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]14
47f : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Uranyl (U⁶⁺) minerals]13
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]4
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits4
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]3
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]3
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)2