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Paragenetic Mode 37 : Layered igneous intrusions and related PGE minerals

Return to the list of paragentic modes

Description

In spite of their affinity to other mafic/ultramafic igneous rocks, we consider layered igneous intrusions to be a separate paragenetic environment because of their unusual homogeneous aerial extent, their predominantly Precambrian ages, and the common occurrence of metal-enriched layers.

Stage

Stage 4b: Highly evolved igneous rocks - Age: >3.0 Ga
34 : Complex granite pegmatites
35 : Ultra-alkali and agpaitic igneous rocks
36 : Carbonatites, kimberlites, and related igneous rocks
37 : Layered igneous intrusions and related PGE minerals

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
Actinolite◻Ca2(Mg4.5-2.5Fe0.5-2.5)Si8O22(OH)2Monoclinic
ArsenopalladinitePd8(As,Sb)3Triclinic
ArsenopyriteFeAsSMonoclinic
AtheneitePd2As0.75Hg0.25Hexagonal
Atokite(Pd,Pt)3SnIsometric
BorniteCu5FeS4Orthorhombic
BowieiteRh2S3Orthorhombic
BowlesitePtSnSOrthorhombic
BraggitePdPt3S4Tetragonal
CabriitePd2CuSnOrthorhombic
CadmiumCdHexagonal
CarrolliteCuCo2S4Isometric
ChalcopyriteCuFeS2Tetragonal
ChengdeiteIr3FeIsometric
CherepanoviteRhAsOrthorhombic
ChromiteFe2+Cr3+2O4Isometric
CobaltiteCoAsSOrthorhombic
CooperitePtSTetragonal
CreraritePt2-x(Bi,Pb)11(S,Se)11Triclinic
Cuproiridsite(Cu,Fe)Ir2S4Isometric
Cuprorhodsite(Cu1+0.5Fe3+0.5)Rh3+2S4Isometric
DiopsideCaMgSi2O6Monoclinic
ErlichmaniteOsS2Isometric
Ferro-edeniteNaCa2Fe2+5(Si7Al)O22(OH)2Monoclinic
Ferro-hornblende◻Ca2(Fe2+4Al)(Si7Al)O22(OH)2Monoclinic
FerronickelplatinumPt2FeNiTetragonal
Frooditeα-PdBi2Monoclinic
GalenaPbSIsometric
GaotaiiteIr3Te8Isometric
Garutiite(Ni,Fe,Ir)Hexagonal
GenkinitePt4Sb3Tetragonal
GersdorffiteNiAsSIsometric
GeversitePtSb2Isometric
GoldAuIsometric
HastingsiteNaCa2(Fe2+4Fe3+)(Si6Al2)O22(OH)2Monoclinic
HaycockiteCu4Fe5S8Orthorhombic
HeazlewooditeNi3S2Trigonal
Hexaferrum(Fe,Os,Ru,Ir)Hexagonal
Hollingworthite(Rh,Pt,Pd)AsSIsometric
HongshiitePtCuTrigonal
InsizwaitePt(Bi,Sb)2Isometric
Irarsite(Ir,Ru,Rh,Pt)AsSIsometric
Iridium(Ir,Os,Ru)Isometric
IsoferroplatinumPt3FeIsometric
IsomertieitePd11Sb2As2Isometric
KaersutiteNaCa2(Mg3AlTi4+)(Si6Al2)O22O2Monoclinic
KeithconnitePd20Te7Trigonal
Kingstonite(Rh,Ir,Pt)3S4Monoclinic
KojonenitePd7-xSnTe2 (0.3 ≤ x ≤ 0.8)Tetragonal
KotulskitePd(Te,Bi)2-x (x ≈ 0.4)Hexagonal
LaflammeitePd3Pb2S2Monoclinic
LauriteRuS2Isometric
LinnaeiteCo2+Co3+2S4Isometric
LukkulaisvaaraitePd14Ag2Te9Tetragonal
MackinawiteFeSTetragonal
MagnesiochromiteMgCr2O4Isometric
MagnetiteFe2+Fe3+2O4Isometric
MajakitePdNiAsHexagonal
MalaniteCu1+(Ir3+Pt4+)S4Isometric
MarathonitePd25Ge9Trigonal
MaslovitePtBiTeIsometric
MeloniteNiTe2Trigonal
MenshikovitePd3Ni2As3Hexagonal
MerenskyitePdTe2Trigonal
MertieitePd8Sb2.5As0.5Trigonal
MiassiteRh17S15Isometric
MicheneritePdBiTeIsometric
MiessiitePd11Te2Se2Isometric
MilleriteNiSTrigonal
MitrofanovitePt3Te4Trigonal
MolybdeniteMoS2Hexagonal
MoncheitePt(Te,Bi)2Trigonal
MooihoekiteCu9Fe9S16Tetragonal
MuskoxiteMg7Fe4O13·10H2OTrigonal
NaldrettitePd2SbOrthorhombic
NickelineNiAsHexagonal
NielsenitePdCu3Tetragonal
NiggliitePtSnHexagonal
OgnititeNiBiTeTrigonal
OrthogersdorffiteNiAsSOrthorhombic
Osarsite(Os,Ru)AsSMonoclinic
Osmium(Os,Ir,Ru)Hexagonal
Oulankaite(Pd,Pt)5(Cu,Fe)4SnTe2S2Tetragonal
PalarstanidePd5(Sn,As)2Hexagonal
Palladium(Pd,Pt)Isometric
PalladoarsenidePd2AsMonoclinic
PalladobismutharsenidePd2(As,Bi)Orthorhombic
Palladodymite(Pd,Rh)2AsOrthorhombic
PalladogermanidePd2GeHexagonal
PalladosilicidePd2SiHexagonal
PaolovitePd2SnOrthorhombic
ParagersdorffiteNi(As,S)2Isometric
Pentlandite(NixFey)Σ9S8Isometric
Percleveite-(Ce)Ce2Si2O7Tetragonal
Percleveite-(La)La2Si2O7Tetragonal
Pigeonite(CaxMgyFez)(Mgy1Fez1)Si2O6Monoclinic
PlatarsitePt(As,S)2Isometric
PlatinumPtIsometric
PlumbopalladinitePd3Pb2Hexagonal
PolaritePd(Bi,Pb)Orthorhombic
PotaritePdHgTetragonal
PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2Monoclinic
PseudomertieitePd11(Sb,As)4Hexagonal
PutoraniteCu1.1Fe1.2S2Isometric
PyriteFeS2Isometric
PyrrhotiteFe1-xSMonoclinic
Rhodarsenide(Rh,Pd)2AsOrthorhombic
Rhodium(Rh,Pt)Isometric
Ruarsite(Ru,Os)AsSMonoclinic
Rustenburgite(Pt,Pd)3SnIsometric
Ruthenarsenite(Ru,Ni)AsOrthorhombic
Rutheniridosmine(Ir,Os,Ru)Hexagonal
Ruthenium(Ru,Ir)Hexagonal
SkaergaarditePdCuIsometric
SobolevskitePdBiHexagonal
SopcheiteAg4Pd3Te4Orthorhombic
SperrylitePtAs2Isometric
SphaleriteZnSIsometric
Stannopalladinite(Pd,Cu)3SnOrthorhombic
StibiopalladinitePd5Sb2Hexagonal
StibniteSb2S3Orthorhombic
StillwateritePd8As3Trigonal
StumpflitePtSbHexagonal
SudburyitePdSbHexagonal
Taimyrite(Pd,Cu,Pt)3SnOrthorhombic
TalnakhiteCu9(Fe,Ni)8S16Isometric
Tarkianite(Cu,Fe)(Re,Mo)4S8Isometric
Telargpalite(Pd,Ag)3(Te,Bi)Isometric
TelluropalladinitePd9Te4Monoclinic
TemagamitePd3HgTe3Trigonal
Tennantite-(Fe)Cu6(Cu4Fe2+2)As4S12SIsometric
Tetra-auricuprideAuCuTetragonal
TetraferroplatinumPtFeTetragonal
TolovkiteIrSbSIsometric
TörnroositePd11As2Te2Isometric
TulameenitePt2CuFeTetragonal
UngavaitePd4Sb3Tetragonal
Vasilite(Pd,Cu)16(S,Te)7Isometric
VincentitePd3AsMonoclinic
ViolariteFe2+Ni3+2S4Isometric
VysotskitePdSTetragonal
Wonesite(Na,K)(Mg,Fe,Al)6((Al,Si)4O10)2(OH,F)4Monoclinic
XingzhongitePb2+Ir3+2S4Isometric
ZaccariniiteRhNiAs Tetragonal
ZincochromiteZnCr2O4Isometric
Zirkelite(Ti,Ca,Zr)O2-xIsometric
ZvyagintsevitePd3PbIsometric
ElementCountPercent
HHydrogen74.76%
OOxygen1711.56%
FFluorine10.68%
NaSodium53.40%
MgMagnesium85.44%
AlAluminium64.08%
SiSilicon128.16%
SSulfur4933.33%
KPotassium10.68%
CaCalcium85.44%
TiTitanium21.36%
CrChromium32.04%
FeIron3322.45%
CoCobalt32.04%
NiNickel1711.56%
CuCopper2214.97%
ZnZinc21.36%
GeGermanium21.36%
AsArsenic3121.09%
SeSelenium21.36%
ZrZirconium10.68%
MoMolybdenum21.36%
RuRuthenium106.80%
RhRhodium117.48%
PdPalladium5436.73%
AgSilver32.04%
CdCadmium10.68%
SnTin117.48%
SbAntimony149.52%
TeTellurium2013.61%
LaLanthanum10.68%
CeCerium10.68%
ReRhenium10.68%
OsOsmium74.76%
IrIridium149.52%
PtPlatinum2919.73%
AuGold21.36%
HgMercury32.04%
PbLead74.76%
BiBismuth128.16%

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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