The Weipu granitic pluton and the Changpu migmatite are developed in the southern part of the Wuyi tectonic belt, South China.
闽西玮埔岩体和赣南菖蒲混合岩位于武夷山构造带南部地区。
The Weipu granitic pluton and the Changpu migmatite are developed in the southern part of the Wuyi tectonic belt, South China.
闽西玮埔岩体和赣南菖蒲混合岩位于武夷山构造带南部地区。
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