Tonalites and plagiogranites of the Char suture-shear zone in East Kazakhstan: Implications for the Kazakhstan-Siberia collision
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文摘

The Char suture-shear zone in East Kazakhstan hosts ca. 323 Ma tonalities and plagiogranites.

These rocks represent high-Al, LREE enriched and HFSE depleted granitoids.

They formed by the melting of lower mafic crust in relation to the Kazakhstan-Siberia collision.

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