Paragenetic Mode 41 : Mantle metasomatism
Return to the list of paragentic modesDescription
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 |
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38 : Ophiolites |
39 : High-π metamorphism (blueschist, eclogite, ultrahigh π 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.
Mineral | Formula | Crystal System |
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Armalcolite | (Mg,Fe2+)Ti2O5 | Orthorhombic |
Barroisite | ◻{CaNa}{Mg3Al2}(AlSi7O22)(OH)2 | Monoclinic |
Carmichaelite | (Ti,Cr,Fe)[O2-x(OH)x] | Monoclinic |
Cordierite | (Mg,Fe)2Al3(AlSi5O18) | Orthorhombic |
Corundum | Al2O3 | Trigonal |
Cummingtonite | ◻{Mg2}{Mg5}(Si8O22)(OH)2 | Monoclinic |
Freudenbergite | Na2(Ti,Fe)8O16 | Monoclinic |
Glaucophane | ◻[Na2][Mg3Al2]Si8O22(OH)2 | Monoclinic |
Ilmenite | Fe2+TiO3 | Trigonal |
Lawsonite | CaAl2(Si2O7)(OH)2·H2O | Orthorhombic |
Nixonite | Na2Ti6O13 | Monoclinic |
Perovskite | CaTiO3 | Orthorhombic |
Priderite | K(Ti4+7Fe3+)O16 | Tetragonal |
Rutile | TiO2 | Tetragonal |
Sekaninaite | (Fe,Mg)2Al3(AlSi5O18) | Orthorhombic |
Zoisite | (CaCa)(AlAlAl)O[Si2O7][SiO4](OH) | Orthorhombic |
Element | Count | Percent | |
---|---|---|---|
H | Hydrogen | 6 | 37.50% |
O | Oxygen | 16 | 100.00% |
Na | Sodium | 4 | 25.00% |
Mg | Magnesium | 6 | 37.50% |
Al | Aluminium | 7 | 43.75% |
Si | Silicon | 7 | 43.75% |
K | Potassium | 1 | 6.25% |
Ca | Calcium | 4 | 25.00% |
Ti | Titanium | 8 | 50.00% |
Cr | Chromium | 1 | 6.25% |
Fe | Iron | 7 | 43.75% |