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Paragenetic Mode 41 : Mantle metasomatism

Return to the list of paragentic modes

Description

Mantle metasomatism is a high-pressure hydrothermal metamorphic process that alters the chemistry of existing ultramafic minerals and produces new phases through interactions with deep C-O-H fluids.

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
Armalcolite(Mg,Fe2+)Ti2O5Orthorhombic
Barroisite◻{CaNa}{Mg3Al2}(AlSi7O22)(OH)2Monoclinic
Carmichaelite(Ti,Cr,Fe)[O2-x(OH)x]Monoclinic
Cordierite(Mg,Fe)2Al3(AlSi5O18)Orthorhombic
CorundumAl2O3Trigonal
Cummingtonite◻{Mg2}{Mg5}(Si8O22)(OH)2Monoclinic
FreudenbergiteNa2(Ti,Fe)8O16Monoclinic
Glaucophane◻[Na2][Mg3Al2]Si8O22(OH)2Monoclinic
IlmeniteFe2+TiO3Trigonal
LawsoniteCaAl2(Si2O7)(OH)2·H2OOrthorhombic
NixoniteNa2Ti6O13Monoclinic
PerovskiteCaTiO3Orthorhombic
PrideriteK(Ti4+7Fe3+)O16Tetragonal
RutileTiO2Tetragonal
Sekaninaite(Fe,Mg)2Al3(AlSi5O18)Orthorhombic
Zoisite(CaCa)(AlAlAl)O[Si2O7][SiO4](OH)Orthorhombic
ElementCountPercent
HHydrogen637.50%
OOxygen16100.00%
NaSodium425.00%
MgMagnesium637.50%
AlAluminium743.75%
SiSilicon743.75%
KPotassium16.25%
CaCalcium425.00%
TiTitanium850.00%
CrChromium16.25%
FeIron743.75%

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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