Predictive Mineralogy
This table is based on statistical analysis of other localities containing similar species to the ones found at this locality.
Possible missing species | Formula | Match % | Due to recorded presence of |
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Chalcopyrite | CuFeS2 | 41.37% | Pyrite (51.72 %) |
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 Mode | Score |
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48 : Soil leaching zone minerals
Unique: Gibbsite | 100 |
47a : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals] | 25 |
47c : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates] | 25 |
49 : Oxic cellular biomineralization (see also #44) | 0 |
24 : Authigenic minerals in terrestrial sediments (see also #17) | 0 |
14 : Hot springs, geysers, and other subaerial geothermal minerals | 0 |
53 : Other minerals with taphonomic origins | 0 |
47h : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals] | 0 |
17 : Marine authigenic Hadean minerals (see also #24) | 0 |
47i : Low-π subaerial oxidative hydration, weathering (see also #16 and #23) - [Terrestrial weathering of meteorites] | 0 |
55 : Anthropogenic mine minerals | 0 |