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岩石学报 1999
Plagioclase xenocryst and magma mingling in Pingtan and Zhangzhou Complexes.
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Abstract:
The magma mingling phenomenon is widely developed in Pingtan and Zhangzhou igneous complexes of SE Fujian. It appears as the existence of gabbro diorite synplutonic dykes and quenched enclaves in the granitic rocks. It is found that there are plagioclas