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Predictive Mineralogy

Possible unrecorded species at Agoudal Centre Quarry, Agoudal Mines, Tansifte Caïdat, Agdz Cercle, Zagora Province, Drâa-Tafilalet Region, Morocco

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
ChalcopyriteCuFeS299.97%Alloclasite (80.28 %), Anorthoroselite (64.00 %), Bariopharmacosiderite (67.20 %), Cobaltaustinite (64.29 %), Erythrite (69.91 %), Lavendulan (64.33 %), Spherocobaltite (67.80 %)
PyriteFeS299.87%Alloclasite (74.65 %), Bariopharmacosiderite (62.90 %), Calcite (51.16 %), Cobaltaustinite (57.14 %), Erythrite (64.88 %), Lavendulan (59.65 %), Spherocobaltite (55.93 %)
MalachiteCu2(CO3)(OH)298.35%Bariopharmacosiderite (65.05 %), Erythrite (51.09 %), Lavendulan (70.18 %), Spherocobaltite (67.80 %)
BaryteBaSO485.03%Bariopharmacosiderite (69.89 %), Lavendulan (50.29 %)
ArsenopyriteFeAsS81.69%Alloclasite (63.38 %), Cobaltaustinite (50.00 %)
OliveniteCu2(AsO4)(OH)79.68%Bariopharmacosiderite (51.08 %), Lavendulan (58.48 %)
AzuriteCu3(CO3)2(OH)278.08%Bariopharmacosiderite (54.30 %), Lavendulan (52.05 %)
GalenaPbS76.40%Alloclasite (54.93 %), Bariopharmacosiderite (53.23 %), Erythrite (53.28 %), Lavendulan (54.39 %)
BrochantiteCu4(SO4)(OH)675.94%Bariopharmacosiderite (51.61 %), Lavendulan (50.29 %)
ConichalciteCaCu(AsO4)(OH)64.28%Cobaltaustinite (64.29 %)
SphaleriteZnS62.68%Alloclasite (56.34 %), Erythrite (50.44 %)
GypsumCaSO4 · 2H2O59.64%Lavendulan (59.65 %)
ArseniosideriteCa2Fe3+3(AsO4)3O2 · 3H2O57.14%Cobaltaustinite (57.14 %)
DolomiteCaMg(CO3)255.93%Spherocobaltite (55.93 %)
CobaltiteCoAsS54.92%Alloclasite (54.93 %)
Goethiteα-Fe3+O(OH)52.68%Bariopharmacosiderite (52.69 %)
SkutteruditeCoAs352.00%Anorthoroselite (52.00 %)
ScoroditeFe3+AsO4 · 2H2O50.00%Cobaltaustinite (50.00 %)

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
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Spherocobaltite
100
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]57
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]57
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])11
55 : Anthropogenic mine minerals1
56 : Slag and smelter minerals (see also #51 and #55)1
10 : Basalt-hosted zeolite minerals0
14 : Hot springs, geysers, and other subaerial geothermal minerals0
35 : Ultra-alkali and agpaitic igneous rocks0
6 : Secondary asteroid phases0
49 : Oxic cellular biomineralization (see also #44)0