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A RAPAKIVI BY ASSIMILATION AND CONTAMINATION IN KUANDIAN, LIAONING PROVINCE, CHINA

Ge Wenchun Lin Qiang Fang Zhanren(Department of Geology)  
Rapakivi is a special rock in Precambrian. This paper has disscussed thegenesis of Proterozoic rapakivi in Kuandian, Liaoning Province of China,ingeology, petrology and mineralogy. We concluded that the rapakivi wasformed by intrusion and crystallization of the crystal-mush magma whichcontained a lot of xenocryst of country rocks Sill-Ga-Bi-Pl-gneisses and Bi-leptynite etc-- The magma was formed by assimilation between a K-richrelict magma of adamellite and its country rock in deepth.The plagioclaseoutercrust of rapakivi feldspar was derived from xenocryst of countryrocks. It surrounded the K-feldspar by flowing and absorption and thusthe rapakivi texture was formed.
【CateGory Index】: P588.1
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