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Paragenetic Mode 51 : Pyrometamorphic minerals (see also #54 and #56)

Return to the list of paragentic modes

Description

Pyrometamorphic minerals of the Hatrurim Formation in the Middle East (Israel and Jordan) include a fascinating suite of species that formed when natural ignition of near-surface hydrocarbon deposits (presumably both natural gas and petroleum) subjected sediments to temperatures in excess of 1000 °C

Age: <0.36 Ga

Stage

Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere - Age: <0.6 Ga
48 : Soil leaching zone minerals
49 : Oxic cellular biomineralization (see also #44)
50 : Coal and/or oil shale minerals
51 : Pyrometamorphic minerals (see also #54 and #56)
52 : Guano- and urine-derived minerals
53 : Other minerals with taphonomic origins

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
AegirineNaFe3+Si2O6Monoclinic
Aegirine-augite(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6Monoclinic
AfwilliteCa3(HSiO4)2·2H2OMonoclinic
ÅkermaniteCa2Mg[Si2O7]Tetragonal
AlbiteNa(AlSi3O8)Triclinic
AlforsiteBa5(PO4)3ClHexagonal
AndraditeCa3Fe3+2(SiO4)3Isometric
AnorthiteCa(Al2Si2O8)Triclinic
AraditeBaCa6[(SiO4)(VO4)](VO4)2FTrigonal
AravaiteBa2Ca18(SiO4)6(PO4)3(CO3)F3OTrigonal
AriegilatiteBaCa12(SiO4)4(PO4)2F2OTrigonal
Augite(CaxMgyFez)(Mgy1Fez1)Si2O6Monoclinic
BarioferriteBaFe3+12O19Hexagonal
Barringerite(Fe,Ni)2PHexagonal
BayeriteAl(OH)3Monoclinic
BennesheriteBa2Fe2+[Si2O7]Tetragonal
BentoriteCa6Cr2(SO4)3(OH)12·26H2OTrigonal
BerzelianiteCu2-xSe (x ≈ 0.12)Isometric
BicchuliteCa2(Al2SiO6)(OH)2Isometric
BredigiteCa7Mg(SiO4)4Orthorhombic
BrownmilleriteCa2(Al,Fe3+)2O5Orthorhombic
BultfonteiniteCa2(HSiO4)F·H2OTriclinic
CalciolangbeiniteK2Ca2(SO4)3 Isometric
ChalcociteCu2SMonoclinic
ChalcopyriteCuFeS2Tetragonal
ChegemiteCa7(SiO4)3(OH)2Orthorhombic
ChlorellestaditeCa5(SiO4)1.5(SO4)1.5ClHexagonal
ChlorkyuygeniteCa12Al14O32[(H2O)4Cl2]Isometric
ChlormayeniteCa12Al14O32[◻4Cl2]Isometric
ChromatiteCaCr6+O4Tetragonal
ChromiteFe2+Cr3+2O4Isometric
ClinohedriteCaZn(SiO4)·H2OMonoclinic
ClintoniteCaAlMg2(SiAl3O10)(OH)2Monoclinic
CopperCuIsometric
CorundumAl2O3Trigonal
CristobaliteSiO2Tetragonal
CuprorivaiteCaCuSi4O10Tetragonal
DargaiteBaCa12(SiO4)4(SO4)2O3Trigonal
DiaoyudaoiteNaAl11O17Hexagonal
DjerfisheriteK6(Fe,Cu,Ni)25S26ClIsometric
DorriteCa4(Mg3Fe3+9)O4(Si3Al8Fe3+O36)Triclinic
DzierżanowskiteCaCu2S2Trigonal
EdgrewiteCa9(SiO4)4F2 Monoclinic
ElbrusiteCa3(U6+0.5Zr1.5)[Fe3+O4]3Isometric
EltyubyuiteCa12Fe3+10Si4O32Cl6Isometric
EsseneiteCaFe3+[AlSiO6]Monoclinic
EttringiteCa6Al2(SO4)3(OH)12·26H2OTrigonal
FlamiteCa8-x(Na,K)x(SiO4)4-x(PO4)xOrthorhombic
FluorkyuygeniteCa12Al14O32[(H2O)4F2]Isometric
FluormayeniteCa12Al14O32F2Isometric
FoshagiteCa4(Si3O9)(OH)2Triclinic
GazeeviteBaCa6(SiO4)2(SO4)2OTrigonal
GehleniteCa2Al[AlSiO7]Tetragonal
GoreriteCaAlFe3+11O19Hexagonal
GrossiteCaAl4O7Monoclinic
GurimiteBa3(VO4)2Trigonal
HalamishiteNi5P4Hexagonal
HarmuniteCaFe2O4Orthorhombic
HashemiteBaCr6+O4Orthorhombic
HatruriteCa3(SiO4)OTrigonal
HexacelsianBaAl2Si2O8Hexagonal
JenniteCa9(Si3O9)2(OH)8·8H2OTriclinic
KahlenbergiteKAl11O17Hexagonal
KalistrontiteK2Sr(SO4)2Trigonal
KalsiliteKAlSiO4Hexagonal
KatoiteCa3Al2[◻(OH)4]3Isometric
KhesiniteCa4(Mg3Fe3+9)O4(Fe3+9Si3)O36Triclinic
KhurayyimiteCa7Zn4(Si2O7)2(OH)10·4H2OMonoclinic
KilchoaniteCa6(SiO4)(Si3O10)Orthorhombic
KumtyubeiteCa5(SiO4)2F2Monoclinic
LakargiiteCa(Zr,Sn,Ti)O3Orthorhombic
LarniteCa2SiO4Monoclinic
LevantiteKCa3Al2(SiO4)(Si2O7)(PO4)Monoclinic
LimeCaOIsometric
LinnaeiteCo2+Co3+2S4Isometric
MagnesiochromiteMgCr2O4Isometric
MagnesioferriteMgFe3+2O4Isometric
MelliteAl2[C6(COO)6]·16H2OTetragonal
MerwiniteCa3Mg(SiO4)2Monoclinic
MolybdeniteMoS2Hexagonal
MonticelliteCaMgSiO4Orthorhombic
MulliteAl4+2xSi2-2xO10-xOrthorhombic
MurashkoiteFePOrthorhombic
NabimusaiteKCa12(SiO4)4(SO4)2O2FTrigonal
NagelschmidtiteCa7(SiO4)2(PO4)2Hexagonal
NataliakulikiteCa4Ti2(Fe3+,Fe2+)(Si,Fe3+,Al)O11Orthorhombic
NazaroviteNi12P5Tetragonal
NegeviteNiP2Isometric
NephelineNa3K(Al4Si4O16)Hexagonal
NickolayiteFeMoPOrthorhombic
OkeniteCa10Si18O46·18H2OTriclinic
Oldhamite(Ca,Mg)SIsometric
OrishchiniteNi2POrthorhombic
OyeliteCa10Si8B2O29·12.5H2OTriclinic
PericlaseMgOIsometric
PliniusiteCa5(VO4)3FHexagonal
Plombièrite[Ca4Si6O16(OH)2·2H2O]·(Ca·5H2O)Orthorhombic
PolekhovskyiteMoNiP2Hexagonal
PortlanditeCa(OH)2Trigonal
Priscillagrewite-(Y)(Ca2Y)Zr2(AlO4)3Isometric
PseudobrookiteFe2TiO5Orthorhombic
PseudowollastoniteCaSiO3Monoclinic
QatranaiteCaZn2(OH)6(H2O)2Monoclinic
RankiniteCa3Si2O7Monoclinic
ReinhardbraunsiteCa5(SiO4)2(OH,F)2Monoclinic
RiversideiteCa5(HSi3O9)2·2H2OOrthorhombic
SchorlomiteCa3Ti2(SiO4)(Fe3+O4)2Isometric
SharyginiteCa3TiFe2O8Orthorhombic
ShulamititeCa3TiFe3+AlO8Orthorhombic
SilicocarnotiteCa5[(SiO4)(PO4)](PO4)Orthorhombic
SpurriteCa5(SiO4)2(CO3)Monoclinic
SrebrodolskiteCa2Fe3+2O5Orthorhombic
StracheriteBaCa6(SiO4)2[(PO4)(CO3)]2FTrigonal
TernesiteCa5(SiO4)2(SO4)Orthorhombic
TransjordaniteNi2PHexagonal
TululiteCa14(Fe3+,Al)(Al,Zn,Fe3+,Si,P,Mn,Mg)15O36Isometric
VanadiumVIsometric
VapnikiteCa2CaUO6Monoclinic
VateriteCaCO3Hexagonal
VorlaniteCa(U6+)O4Isometric
WalstromiteBaCa2(Si3O9)Triclinic
Ye'elimiteCa4Al6(SO4)O12Isometric
ZadoviteBaCa6[(SiO4)(PO4)](PO4)2FTrigonal
ZincochromiteZnCr2O4Isometric
Zoharite(Ba,K)6(Fe,Cu,Ni)25S27Isometric
ZuktamruriteFeP2Orthorhombic
ElementCountPercent
HHydrogen2318.25%
BBoron10.79%
CCarbon53.97%
OOxygen10583.33%
FFluorine1310.32%
NaSodium64.76%
MgMagnesium1411.11%
AlAluminium3225.40%
SiSilicon6249.21%
PPhosphorus2015.87%
SSulfur1814.29%
ClChlorine64.76%
KPotassium107.94%
CaCalcium8365.87%
TiTitanium64.76%
VVanadium43.17%
CrChromium64.76%
MnManganese10.79%
FeIron3023.81%
CoCobalt10.79%
NiNickel97.14%
CuCopper86.35%
ZnZinc53.97%
SeSelenium10.79%
SrStrontium10.79%
YYttrium10.79%
ZrZirconium32.38%
MoMolybdenum32.38%
SnTin10.79%
BaBarium1511.90%
UUranium32.38%

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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