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《Acta Petrologica Sinica》 2001-01
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Eclogite facies garnet-pyroxenolite xenolith in Hannuoba area: New evidence of magma underplating

FAN QiCheng, SUI JianLi, LIU RuoXin and ZHOU XinMin.1. Institute of Geology, China Seismological Bureau, Beijing 100029, China; 2. Department of Earth Sciences, Nanjing University, Nanjing 210093, China.  
Eclogite facies garnet pyroxenolite xenoliths in Hannuoba area show the typical layered cumulate structures and crystalloblastic textures of granulite facies. The mineral compositions, equilibrated P T conditions and REE geochemistry of the xnolith reveal its mantle derived genesis. All these facts indicate that the mantle derived magma underplates in the top of the upper mantle and forms the mafic cumulate, then the cumulate experiences some metamorphism of eclogite facies. The eclogite facies xenolith, accomponied with the granulite facies xenolith, provides new evidence of the existence of the crust mantle transitional zone.
【Fund】: 国家自然科学基金项目 (编号 :49772 112 );; 中国科学院知识创新工程项目 (编号 :KZCX1-0 7-0 5 )
【CateGory Index】: P588.1
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