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Predictive Mineralogy

Possible unrecorded species at Trans-Atlantic Geotraverse hydrothermal field (TAG), Mid-Atlantic Ridge complex, Atlantic Ocean

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
MalachiteCu2(CO3)(OH)299.98%Atacamite (56.96 %), Botallackite (57.89 %), Chalcocite (56.20 %), Covellite (54.66 %), Cuprite (79.07 %), Digenite (54.15 %), Idaite (59.75 %), Paratacamite (57.89 %), Tenorite (73.13 %)
AzuriteCu3(CO3)2(OH)276.78%Cuprite (51.54 %), Tenorite (52.10 %)
BrochantiteCu4(SO4)(OH)657.89%Botallackite (57.89 %)
ConnelliteCu19(SO4)(OH)32Cl4 · 3H2O54.38%Botallackite (54.39 %)
SilverAg50.31%Acanthite (50.32 %)

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
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Nukundamite
100
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])38
6 : Secondary asteroid phases23
49 : Oxic cellular biomineralization (see also #44)18
26 : Hadean detrital minerals14
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]10
50 : Coal and/or oil shale minerals9
54 : Coal and other mine fire minerals (see also #51 and #56)8
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)8
45b : Oxidized fumarolic minerals (see also [#11]) - [Other oxidized fumarolic minerals]6
13 : Hadean serpentinization6