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Predictive Mineralogy

Possible unrecorded species at Artenberg quarry, Steinach, Haslach im Kinzigtal, Ortenaukreis, Freiburg Region, Baden-Württemberg, Germany

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
BrochantiteCu4(SO4)(OH)685.95%Antlerite (70.65 %), Cornwallite (52.15 %)
UraniniteUO276.64%Coffinite (76.64 %)
DiopsideCaMgSi2O676.39%Grossular (52.27 %), Wollastonite (50.54 %)
OliveniteCu2(AsO4)(OH)74.16%Cornwallite (74.16 %)
ValentiniteSb2O368.59%Senarmontite (68.60 %)
CovelliteCuS59.04%Antlerite (59.04 %)
CupriteCu2O51.53%Antlerite (51.54 %)
AcanthiteAg2S50.60%Pyrargyrite (50.61 %)
JamesonitePb4FeSb6S1450.00%Fülöppite (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
33 : Minerals deposited by hydrothermal metal-rich fluids (see also [#12])

Unique: Boulangerite, Bournonite, Fülöppite, Plagionite, Pyrargyrite, Semseyite, etc.
623
47h : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]

Unique: Wulfenite
100
47a : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]46
47d : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]34
47c : Low-𝑇 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]22
53 : Other minerals with taphonomic origins19
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)17
6 : Secondary asteroid phases13
34 : Complex granite pegmatites12
31 : Thermally altered carbonate, phosphate, and iron formations12
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)10
50 : Coal and/or oil shale minerals9