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Paragenetic Mode 39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)

Return to the list of paragentic modes

Description

Plate tectonic processes have also led to the exposure of metamorphic rocks from environments with unusually low-geothermal gradients, estimated to be <10 °C/km—conditions only possible during relatively rapid subduction of crustal rocks to great depths, with subsequent buoyant uplift.

Stage

Stage 5: Initiation of plate tectonics - Age: <3.5-2.5 Ga
38 : Ophiolites
39 : High-𝑃 metamorphism (blueschist, eclogite, ultrahigh 𝑃 facies)
40 : Regional metamorphism (greenschist, amphibolite, granulite facies)
41 : Mantle metasomatism
42 : Sea-floor Mn nodules
43 : Shear-induced minerals (including mylonite/slickensides)

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
AegirineNaFe3+Si2O6Monoclinic
Aegirine-augite(NaaCabFe2+cMgd)(Fe3+eAlfFe2+gMgh)Si2O6Monoclinic
AluminoceladoniteK(MgAl◻)(Si4O10)(OH)2Monoclinic
AragoniteCaCO3Orthorhombic
BarioperovskiteBaTiO3Orthorhombic
Barroisite◻{CaNa}{Mg3Al2}(AlSi7O22)(OH)2Monoclinic
BearthiteCa2Al(PO4)2(OH)Monoclinic
BreyiteCa3Si3O9Triclinic
Bridgmanite(Mg,Fe)SiO3Orthorhombic
CarpholiteMn2+Al2(Si2O6)(OH)4Orthorhombic
Chloritoid(Fe2+,Mg,Mn2+)Al2(SiO4)O(OH)2Monoclinic
Clinozoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)Monoclinic
CoesiteSiO2Monoclinic
CorundumAl2O3Trigonal
Cummingtonite◻{Mg2}{Mg5}(Si8O22)(OH)2Monoclinic
Deerite(Fe,Mn)6(Fe,Al)3[Si6O17]O3(OH)5Monoclinic
DonwilhelmsiteCaAl4Si2O11Hexagonal
EllenbergeriteMg6(Mg,Ti,Zr,◻)2(Al,Mg)6Si8O28(OH)10Hexagonal
EnstatiteMg2Si2O6Orthorhombic
Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)Monoclinic
Epidote-(Sr)(CaSr)(AlAlFe3+)O[Si2O7][SiO4](OH)Monoclinic
Ferro-actinolite◻Ca2Fe2+5(Si8O22)(OH)2Monoclinic
Ferro-glaucophane◻[Na2][Fe2+3Al2]Si8O22(OH)2Monoclinic
Ferro-katophorite{Na}{CaNa}{Fe2+4Al}[(AlSi7)O22](OH)2Monoclinic
Ferro-taramiteNa(CaNa)(Fe2+3Al2)(Al2Si6O22)(OH)2Monoclinic
FerrocarpholiteFe2+Al2Si2O6(OH)4Orthorhombic
Fluoro-taramite{Na}{CaNa}{Mg3Al2}(Al2Si6O22)F2Monoclinic
GalaxiteMn2+Al2O4Isometric
Glaucophane◻[Na2][Mg3Al2]Si8O22(OH)2Monoclinic
HiroseiteFeSiO3Orthorhombic
HowieiteNa(Fe,Mn)10(Fe,Al)2Si12O31(OH)13Triclinic
HydroxylwagneriteMg2(PO4)(OH)Monoclinic
ItoigawaiteSrAl2(Si2O7)(OH)2·H2OOrthorhombic
JadeiteNa(Al,Fe3+)Si2O6Monoclinic
Katophorite{Na}{CaNa}{Mg4Al}[(AlSi7)O22](OH)2Monoclinic
KokchetaviteK(AlSi3O8)Hexagonal
KumdykoliteNa(AlSi3O8)Orthorhombic
KyaniteAl2(SiO4)OTriclinic
LawsoniteCaAl2(Si2O7)(OH)2·H2OOrthorhombic
MagnesiochloritoidMgAl2(SiO4)O(OH)2Monoclinic
MagnesiostauroliteMg(Mg,Li)3(Al,Mg)18Si8O44(OH)4Monoclinic
MagnesiteMgCO3Trigonal
MajoriteMg3(MgSi)(SiO4)3Isometric
MaruyamaiteK(Al2Mg)(Al5Mg)(Si6O18)(BO3)3(OH)3OTrigonal
MavlyanoviteMn5Si3Hexagonal
MoissaniteSiCHexagonal
Omphacite(NaaCabFe2+cMgd)(AleFe3+fFe2+gMgh)Si2O6Monoclinic
Ottrélite(Mn2+,Fe2+,Mg)Al2(SiO4)O(OH)2Monoclinic
ParagoniteNaAl2(AlSi3O10)(OH)2Monoclinic
PrehniteCa2Al2Si3O10(OH)2Orthorhombic
Pumpellyite-(Al)Ca2Al3(Si2O7)(SiO4)(OH,O)2·H2OMonoclinic
PyropeMg3Al2(SiO4)3Isometric
QingsongiteBNIsometric
QusongiteWCHexagonal
RutileTiO2Tetragonal
SanidineK(AlSi3O8)Monoclinic
Stilpnomelane(K,Ca,Na)(Fe,Mg,Al)8(Si,Al)12(O,OH)36·nH2OTriclinic
TalcMg3Si4O10(OH)2Triclinic
Taneyamalite(Na,Ca)(Mn,Mg,Fe)12Si12(O,OH)44Triclinic
TaramiteNa(CaNa)(Mg3Al2)(Al2Si6O22)(OH)2Monoclinic
TistariteTi3+2O3Trigonal
TrinephelineNaAlSiO4 Hexagonal
Tschermakite◻(Ca2)(Mg3Al2)(Al2Si6O22)(OH)2Monoclinic
Wagnerite(Mg,Fe2+)2(PO4)FMonoclinic
WernerkrauseiteCa(Fe3+,Mn3+)2Mn4+O6Orthorhombic
Winchite◻{CaNa}{Mg4Al}(Si8O22)(OH)2Monoclinic
ZagamiiteCaAl2Si3.5O11Hexagonal
Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)Orthorhombic
ElementCountPercent
HHydrogen3753.62%
LiLithium11.45%
BBoron22.90%
CCarbon45.80%
NNitrogen11.45%
OOxygen6594.20%
FFluorine22.90%
NaSodium1927.54%
MgMagnesium2840.58%
AlAluminium4565.22%
SiSilicon5681.16%
PPhosphorus34.35%
KPotassium57.25%
CaCalcium2739.13%
TiTitanium45.80%
MnManganese913.04%
FeIron2231.88%
SrStrontium22.90%
ZrZirconium11.45%
BaBarium11.45%
WTungsten11.45%

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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