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Predictive Mineralogy

Possible unrecorded species at Yangshuo Mine, Yangshuo Co., Guilin, Guangxi, China

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
PyriteFeS299.99%Baryte (50.79 %), Calcite (51.16 %), Cerussite (56.77 %), Chalcopyrite (75.16 %), Dolomite (58.22 %), Galena (66.84 %), Hematite (50.17 %), Malachite (52.79 %), Plumbogummite (64.36 %), Pyromorphite (55.98 %), Sphalerite (75.10 %)

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
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]50
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits33
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]33
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]33
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]16
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]16
53 : Other minerals with taphonomic origins12
47g : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Halogen-bearing surface weathering minerals]9
57 : Other minerals formed by human processes4
47e : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Vanadates, chromates, manganates]4