An experimental study of carbonated eclogite at 3·5-5·5 GPa-implications for silicate and carbonate metasomatism in the cratonic mantle
We have experimentally investigated a K-bearing altered mid-ocean ridge basalt (MORB) composition to which 10% CaCO 3 was added (GA1 + 10%cc), at temperatures of 1050-1400°C and pressures of 3·5-5·5 GPa. Experiments were conducted in piston-cylinder ap
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|Source:||Journal of Petrology|
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