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Predictive Mineralogy

Possible unrecorded species at St. Lawrence County, New York, USA

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
SpessartineMn2+3Al2(SiO4)397.03%Clino-suenoite (79.49 %), Kanoite (66.67 %), Pyroxmangite (56.63 %)
RhodochrositeMnCO396.75%Clino-suenoite (70.09 %), Pyroxmangite (74.70 %), Turneaureite (57.14 %)
CupriteCu2O94.96%Botallackite (50.88 %), Namuwite (68.49 %), Nantokite (67.50 %)
CopperCu86.84%Namuwite (56.16 %), Nantokite (70.00 %)
TephroiteMn2+2SiO484.93%Kanoite (66.67 %), Pyroxmangite (54.82 %)
AragoniteCaCO384.81%Hydrotalcite (55.66 %), Namuwite (65.75 %)
DigeniteCu9S583.37%Geerite (55.32 %), Spionkopite (62.79 %)
StibniteSb2S381.55%Cervantite (81.55 %)
BerylBe3Al2(Si6O18)78.64%Chrysoberyl (57.29 %), Isokite (50.00 %)
BournonitePbCuSbS376.75%Geocronite (53.50 %), Sartorite (50.00 %)
LinaritePbCu(SO4)(OH)275.34%Namuwite (75.34 %)
YarrowiteCu9S870.93%Spionkopite (70.93 %)
SerpieriteCa(Cu,Zn)4(SO4)2(OH)6 路 3H2O67.12%Namuwite (67.12 %)
PyrophaniteMn2+TiO366.66%Kanoite (66.67 %)
Schulenbergite(Cu,Zn)7(SO4)2(OH)10 路 3H2O65.75%Namuwite (65.75 %)
Aurichalcite(Zn,Cu)5(CO3)2(OH)660.27%Namuwite (60.27 %)
LangiteCu4(SO4)(OH)6 路 2H2O60.27%Namuwite (60.27 %)
PyrolusiteMn4+O258.97%Groutite (58.97 %)
FrankliniteZn2+Fe3+2O457.14%Turneaureite (57.14 %)
JohannseniteCaMn2+Si2O657.14%Turneaureite (57.14 %)
Todorokite(Na,Ca,K,Ba,Sr)1-x(Mn,Mg,Al)6O12 路 3-4H2O57.14%Turneaureite (57.14 %)
AnalcimeNa(AlSi2O6) 路 H2O56.37%Natrolite (56.38 %)
ConnelliteCu19(SO4)(OH)32Cl4 路 3H2O54.38%Botallackite (54.39 %)
Cordierite(Mg,Fe)2Al3(AlSi5O18)54.34%Grandidierite (54.35 %)
ManganiteMn3+O(OH)53.84%Groutite (53.85 %)
Xenotime-(Y)Y(PO4)53.22%Synchysite-(Y) (53.23 %)
PosnjakiteCu4(SO4)(OH)6 路 H2O52.05%Namuwite (52.05 %)
MilleriteNiS51.19%Siegenite (51.19 %)
BruciteMg(OH)250.94%Hydrotalcite (50.94 %)
EnargiteCu3AsS450.00%Sartorite (50.00 %)
ForsteriteMg2SiO450.00%Warwickite (50.00 %)
WitticheniteCu3BiS345.71%Turneaureite (57.14 %)

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, Dufr茅noysite, Freibergite Subgroup, Geerite, Pyrargyrite, Sartorite
613
31 : Thermally altered carbonate, phosphate, and iron formations

Unique: Lazurite
230
23 : Subaerial aqueous alteration by non-redox-sensitive fluids (see also #47)

Unique: Serendibite
175
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)127
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)

Unique: Siegenite
116
47c : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Carbonates, phosphates, borates, nitrates]

Unique: Smithsonite
112
13 : Hadean serpentinization

Unique: Hydrotalcite
102
10 : Basalt-hosted zeolite minerals

Unique: Stellerite
100
34 : Complex granite pegmatites75
32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits60
26 : Hadean detrital minerals45
47h : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface oxidized, dehydrated minerals]40
47a : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Near-surface hydration of prior minerals]36
35 : Ultra-alkali and agpaitic igneous rocks29
47d : Low-饾憞 subaerial oxidative hydration, weathering (see also #16 and #23) - [Arsenates, antimonates, selenates, bismuthinates]27
36 : Carbonatites, kimberlites, and related igneous rocks23
49 : Oxic cellular biomineralization (see also #44)16