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Early Paleozoic subduction processes of the Paleo-Asian Ocean: Insights from geochronology and geochemistry of Paleozoic plutons in the Alxa Terrane
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文摘

458–407 Ma diorites and granitoids were recognized in the Alxa Terrane.

458–440 Ma and 417–407 Ma groups have different geochemistry and petrogeneses.

Southward subduction of the Paleo-Asian Ocean commenced in the early Paleozoic.

A tectonic switch from advancing to retreating subduction occurred at ~ 407 Ma.

The Alxa had a close link with the North China Craton since the early Paleozoic.

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