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This page is a summary of: The origin of mafic microgranular enclaves and their host granodiorites from East Kunlun, Northern Qinghai-Tibet Plateau: implications for magma mixing during subduction of Paleo-Tethyan lithosphere, Mineralogy and Petrology, December 2011, Springer Science + Business Media,
DOI: 10.1007/s00710-011-0187-1.
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