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《Journal of Jiling University (Earth Science Edition)》 1993-03
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DISCOVERY COESITE IN ECLOGUE AND KYANITE QUARTZITE FROM THE DABIE MOUNTAINS,HENAN PROVINCE

Li Xucxie Rang Weiguo Xu Peicang(Changchun Univ of Earth Sciences) (Xi'an Institute of Geoloy and Mineral Resources)  
Coesite has been first discovered in the eclogites and their country rocks -kyanite quartzite in the western area of Tuanma Fault from the Dabie Mountains , Henan province. The mineral assemblage in the eclogites is garnet + omphacite + kyanite+ phengite+quartz (coesite)+rutile. The coesite - bearing eclogites were estimated to be formed at T=610-740℃ , P≥2. 8 GPa. The coesite-bearing eclogites and their country rocks underwent simultaneously ultra - high - pressure metamorphism. They might be produced by subduction to depths of more than 90km during continent - continent collision between Yangtze and the North China cratons. The discovery of coesite -bearing eclogites in this area enlarges the region of coesite-bearing eclogite belt in Central -Eastern China.
【CateGory Index】: P588.3
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