Melting the lithosphere: Metasomes as a source for mantle-derived magmas
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文摘
High- and low-Ti lava types found in a ∼24 Ma shield volcano on the Ethiopian Plateau. Low-Ti lavas are derived from a source similar to those in the Ethiopian rift. High-Ti lavas are melts of an amphibole-rich lithospheric metasome. Thermobaric destabilization of mantle metasomes may facilitate lithospheric thinning.

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