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Paleoarchean mantle hydrous reservoir beneath South Africa?.
Asafov, E. V., Sobolev, A. V., Gurenko, A. A., Arndt, N. T., Batanova, V. G., Portnyagin, Maxim V. , Garbe-Schönberg, D., Krasheninnikov, S. P., Wilson, A. H. and Byerly, G. R.
(2016)
Paleoarchean mantle hydrous reservoir beneath South Africa?.
[Talk]
In: Goldschmidt Conference 2016. , 26.06-01.07.2016, Yokohama, Japan .
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Abstract
Recent study of melt inclusions in high magnesian olivines (Fo 92.4-Fo 94.2) from the 2.7 Ga komatiites of the Abitibi Greenstone Belt, Canada [Sobolev et al, Nature, 2016] demonstrates an early contamination of melts by seawater brines indicated by elevated concentrations of Cl. Yet the melt inclusions in the most magnesian olivines (Fo 94-94.5) that have not been affected by the seawater contain up to 0.8 wt.% H2O suggesting presence of hydrous reservoir in the deep mantle at Neoarchean time. The present contribution may extend the age of this reservoir by 800
million years...
Document Type: | Conference or Workshop Item (Talk) |
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Keywords: | Paleoarchean mantle, hydrous reservoir, South Africa, olivine |
Research affiliation: | Kiel University OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-MUHS Magmatic and Hydrothermal Systems |
Date Deposited: | 08 Nov 2016 11:13 |
Last Modified: | 08 Nov 2016 11:13 |
URI: | https://oceanrep.geomar.de/id/eprint/34588 |
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