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Paleo-Asian oceanic subduction-related modification of the lithospheric mantle under the North China Craton: Evidence from peridotite xenoliths in the Datong basalts
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文摘

Peridotite xenoliths in the Datong Quaternary alkaline basalt are studied.

In-situ analysis of clinopyroxenes in the peridotite xenoliths indicates carbonatitic metasomatism.

Agent for carbonatitic metasomatism was derived from subducted carbonated pelite.

Subduction of the Paleo-Asian oceanic plate could have contributed to the carbonatitic metasomatism.

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