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Sodium-rich metasomatism in the upper mantle: implications of experiments on the pyrolite-Na/sub 2/O-rich fluid system at 950/sup 0/C, 20 kbar

Journal Article · · Geochim. Cosmochim. Acta; (United States)
Sodium-rich metasomatism in the upper levels of the mantle has been modeled by reacting pyrolite with alkali-bearing H/sub 2/O fluids containing minor CO/sub 2/ and concentrations of Na/sub 2/O and Na/sub 2/O + K/sub 2/O (K/K + Na = 0.1) up to 4.0 g alkalies/10 g H/sub 2/O at 20 kbar and 950/sup 0/C. With increasing alkali concentration, the amounts of amphibole (pargasite-edenite) and olivine increase as orthopyroxene and clinopyroxene decrease. Amphiboles show progressive increases in Na (and K) and Si concentrations and decreases in Al and Ca concentrations suggesting the dominant substitution mechanism is (Na, K) + Si in equilibrium Al + Ca. These results and least squares mass balance calculations suggest the reaction of clinopyroxene + orthopyroxene + spinel produces amphibole + olivine. The present study suggest that up to 43 wt.% amphibole may be accommodated in pyrolite in the presence of Na/sub 2/O-rich H/sub 2/O-CO/sub 2/ fluids. This represents 0.8 wt.% H/sub 2/O and 1.7 wt.% Na/sub 2/O in the hydrated pyrolite composition and indicates the importance of sodium in determining the extent of metasomatism. Sodium also lowers the solidus temperature of pyrolite by more than 50/sup 0/C over the H/sub 2/O-saturated pyrolite system at 20 kbar.
Research Organization:
Univ. of Western Ontario, London (Canada)
OSTI ID:
5100184
Journal Information:
Geochim. Cosmochim. Acta; (United States), Journal Name: Geochim. Cosmochim. Acta; (United States) Vol. 51:9; ISSN GCACA
Country of Publication:
United States
Language:
English