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

Return to the list of paragentic modes

Description

Subsurface Hadean hydrothermal sulfide deposits represent an important yet enigmatic early source of mineral diversity. Today, hydrothermal systems boast more than 850 species of sulfides, arsenides, antimonides, and a wide range of sulfosalts bearing relatively rare elements such as Ge, Sn, Bi, Se, and Te. However, Hazen et al postulate that these uncommon elements were not sufficiently concentrated in Hadean hydrothermal fluids to generate such a wide range of compounds.

Stage

Stage 3b: Earth’s earliest hydrosphere - Age: >4.45 Ga
12 : Hadean hydrothermal subsurface sulfide deposits (see also #33)
13 : Hadean serpentinization
14 : Hot springs, geysers, and other subaerial geothermal minerals
15 : Black/white smoker minerals and other seafloor hydrothermal minerals
16 : Low-𝑇 aqueous alteration of Hadean subaerial lithologies (see also #23)
17 : Marine authigenic Hadean minerals (see also #24)
18 : Minerals formed by freezing

Minerals

Click on a button to filter by elements. Green = must include. Black = must exclude. Mineral names listed in bold are exclusively known from this paragenetic mode.

MineralFormulaCrystal System
AlabanditeMnSIsometric
AlacrániteAs8S9Monoclinic
ArsenopyriteFeAsSMonoclinic
Atokite(Pd,Pt)3SnIsometric
BarquilliteCu2CdGeS4Tetragonal
BismuthiniteBi2S3Orthorhombic
BorniteCu5FeS4Orthorhombic
BowieiteRh2S3Orthorhombic
BowlesitePtSnSOrthorhombic
BraggitePdPt3S4Tetragonal
BriartiteCu2(Fe,Zn)GeS4Tetragonal
BunseniteNiOIsometric
CannizzaritePb48Bi56S132Monoclinic
CattieriteCoS2Isometric
ČernýiteCu2(Cd,Zn,Fe)SnS4Tetragonal
ChalcociteCu2SMonoclinic
ChalcopyriteCuFeS2Tetragonal
CinnabarHgSTrigonal
CobaltpentlanditeCo9S8Isometric
CooperitePtSTetragonal
CopperCuIsometric
CovelliteCuSHexagonal
Cuproiridsite(Cu,Fe)Ir2S4Isometric
Cuprorhodsite(Cu1+0.5Fe3+0.5)Rh3+2S4Isometric
DamiaoitePtIn2Isometric
DaomaniteCuPtAsS2Orthorhombic
DigeniteCu9S5Trigonal
DjerfisheriteK6(Fe,Cu,Ni)25S26ClIsometric
DjurleiteCu31S16Monoclinic
EdeniteNaCa2Mg5(Si7Al)O22(OH)2Monoclinic
EnstatiteMg2Si2O6Orthorhombic
FamatiniteCu3SbS4Tetragonal
FerrokësteriteCu2FeSnS4Tetragonal
FukuchiliteCu3FeS8Isometric
GabrieliteTl6Ag3Cu6(As,Sb)9S21Triclinic
GalenaPbSIsometric
GalenobismutitePbBi2S4Orthorhombic
GalliteCuGaS2Tetragonal
GeocronitePb14Sb6S23Monoclinic
GilaliteCu5Si6O17·7H2OMonoclinic
Godlevskite(Ni,Fe)9S8Orthorhombic
GoldAuIsometric
GratonitePb9As4S15Trigonal
GreenockiteCdSHexagonal
GustaviteAgPbBi3S6Orthorhombic
HeazlewooditeNi3S2Trigonal
HemusiteCu6SnMoS8Isometric
HeyrovskýitePb6Bi2S9Orthorhombic
HocartiteAg2(Fe2+,Zn)SnS4Tetragonal
HoromaniteFe6Ni3S8Tetragonal
InaglyiteCu3Pb(Ir,Pt)8S16Hexagonal
InditeFeIn2S4Isometric
IsocubaniteCuFe2S3Isometric
JordanitePb14As6S23Monoclinic
JordisiteMoS2Amorphous
KësteriteCu2ZnSnS4Tetragonal
KeutschiteCu2AgAsS4Tetragonal
Kharaelakhite(Cu,Pt,Pb,Fe,Ni)9S8Orthorhombic
Kingstonite(Rh,Ir,Pt)3S4Monoclinic
KirkiitePb10Bi3As3S19Monoclinic
KonderiteCu3Pb(Rh,Pt,Ir)8S16Hexagonal
KuramiteCu3SnS4Tetragonal
LaflammeitePd3Pb2S2Monoclinic
LillianitePb3-2xAgxBi2+xS6Orthorhombic
LinnaeiteCo2+Co3+2S4Isometric
LisiguangitePtCuBiS3Orthorhombic
LöllingiteFeAs2Orthorhombic
LuzoniteCu3AsS4Tetragonal
MackinawiteFeSTetragonal
MalaniteCu1+(Ir3+Pt4+)S4Isometric
MarcobaldiitePb12(Sb3As2Bi)Σ6S21Triclinic
MetastibniteSb2S3Amorphous
MiassiteRh17S15Isometric
MilleriteNiSTrigonal
MolybdeniteMoS2Hexagonal
MozgovaitePbBi4S7Orthorhombic
NukundamiteCu3.33Fe0.66S4Trigonal
OberthüriteRh3Ni32S32Isometric
Omphacite(NaaCabFe2+cMgd)(AleFe3+fFe2+gMgh)Si2O6Monoclinic
OrpimentAs2S3Monoclinic
Owensite(Ba,Pb)6(Cu,Fe,Ni)25S27Isometric
PararealgarAs4S4Monoclinic
PargasiteNaCa2(Mg4Al)(Si6Al2)O22(OH)2Monoclinic
Pentlandite(NixFey)Σ9S8Isometric
PermingeatiteCu3SbSe4Tetragonal
PirquitasiteAg2ZnSnS4Tetragonal
Polhemusite(Zn,Hg)STetragonal
PolydymiteNi2+Ni3+2S4Isometric
Potassic-chloro-hastingsiteKCa2(Fe2+4Fe3+)(Si6Al2)O22Cl2Monoclinic
Potassic-hastingsiteKCa2(Fe2+4Fe3+)(Al2Si6O22)(OH)2Monoclinic
PyriteFeS2Isometric
PyrrhotiteFe1-xSMonoclinic
RambergiteMnSHexagonal
RealgarAs4S4Monoclinic
RheniiteReS2Triclinic
RhodplumsiteRh3Pb2S2Trigonal
RichardsiteZn2CuGaS4Tetragonal
RoxbyiteCu9S5Triclinic
Rudashevskyite(Fe,Zn)SIsometric
Rustenburgite(Pt,Pd)3SnIsometric
RutileTiO2Tetragonal
SamaniiteCu2Fe5Ni2S8Tetragonal
SiegeniteCoNi2S4Isometric
SphaleriteZnSIsometric
SpionkopiteCu39S28Hexagonal
StanniteCu2FeSnS4Tetragonal
StaročeskéiteAg0.70Pb1.60(Bi1.35Sb1.35)Σ2.70S6Orthorhombic
Stilbite-NaNa9(Si27Al9)O72·28H2OMonoclinic
SugakiiteCu(Fe,Ni)8S8Tetragonal
SulfhydrylbystriteNa5K2Ca[Al6Si6O24](S5)2(SH)Trigonal
Tarkianite(Cu,Fe)(Re,Mo)4S8Isometric
TerrywallaceiteAgPb(Sb,Bi)3S6 Monoclinic
ThalfenisiteTl6(Fe,Ni,Cu)25S26ClIsometric
UchucchacuaiteAgMnPb3Sb5S12Orthorhombic
VaesiteNiS2Isometric
VelikiteCu2HgSnS4Tetragonal
Villamanínite(Cu,Ni,Co,Fe)S2Triclinic
ViolariteFe2+Ni3+2S4Isometric
VysotskitePdSTetragonal
Westerveldite(Fe,Ni,Co)AsOrthorhombic
WittitePb9Bi12(S,Se)27Monoclinic
Wurtzite(Zn,Fe)SHexagonal
WuyanzhiiteCu2STetragonal
XilingolitePb3Bi2S6Monoclinic
XingzhongitePb2+Ir3+2S4Isometric
YarrowiteCu9S8Trigonal
ZincobriartiteCu2(Zn,Fe)(Ge,Ga)S4Tetragonal
ZvyagintsevitePd3PbIsometric
ElementCountPercent
HHydrogen64.69%
OOxygen118.59%
NaSodium53.91%
MgMagnesium43.13%
AlAluminium75.47%
SiSilicon97.03%
SSulfur10985.16%
ClChlorine32.34%
KPotassium43.13%
CaCalcium64.69%
TiTitanium10.78%
MnManganese32.34%
FeIron3728.91%
CoCobalt64.69%
NiNickel1914.84%
CuCopper4736.72%
ZnZinc118.59%
GaGallium32.34%
GeGermanium32.34%
AsArsenic1511.72%
SeSelenium21.56%
MoMolybdenum43.13%
RhRhodium75.47%
PdPalladium64.69%
AgSilver97.03%
CdCadmium32.34%
InIndium21.56%
SnTin129.38%
SbAntimony97.03%
BaBarium10.78%
ReRhenium21.56%
IrIridium64.69%
PtPlatinum129.38%
AuGold10.78%
HgMercury32.34%
TlThallium21.56%
PbLead2519.53%
BiBismuth1410.94%

References

Hazen, Robert M., Morrison, Shaunna M. (2022) On the paragenetic modes of minerals: A mineral evolution perspective. American Mineralogist, 107 (7) 1262-1287 doi:10.2138/am-2022-8099
 
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