Experimental phase and melting relations of metapelite in the upper mantle: implications for the petrogenesis of intraplate magmas
We performed a series of piston-cylinder experiments on a synthetic pelite starting material over a pressure and temperature range of 3.0-5.0 GPa and 1,100-1,600°C, respectively, to examine the melting behaviour and phase relations of sedimentary rocks a
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|Source:||Contributions to Mineralogy and Petrology|
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