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《Geochimica》 2007-02
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Water in Neoarchean and Mesozoic lower continental crust, North China: A case study from Hannuoba

YANG Xiao-zhi1 , XIA Qun-ke1, FAN Qi-cheng2, Etienne Deloule3 and HAO Yan-tao11. School of Earth and Space Sciences, University of Science and Technology of China, Key Laboratory of Crust-Mantle Materials and Environments, University of Science and Technology of China, Chinese Academy of Sciences, Hefei 230026, China; 2. Institute of Geology, China Earthquake Administration, Beijing 100029, China;3. CRPG-CNRS, Nancy, France  
Nominally anhydrous minerals (clinopyroxene, orthopyroxene, plagioclase and garnet) within Archean terrain granulites and xenolith granulites captured by Cenozoic basalts from Hannuoba, North China are investigated by Fourier Transform Infrared spectroscopy (FTIR). The results show that all these minerals can contain some water in the manner of OH. Calculated water contents are highly variable, indicating that the water distribution in the lower crust is very likely heterogeneous. However, the water contents of minerals in terrain granulites are obviously higher, by a factor of ~ 2, than those in xenolith granulites, but similar to those in Nü shan xenolith granulites (Yang et al., 2005). The water contrast between terrain and xenolith granulites suggests that the early (Neoarchean to Paleoproterozoic) lower crust is probably more hydrous than that formed in Mesozoic, implying that different nature and formation mechanisms are involved for the lower crust built in different times.
【Fund】: 国家自然科学基金(40673028 40473007);; 中法先进研究计划(PRAT05-02);; 教育部“新世纪优秀人才支持计划”;; 中国科学院研究生科学与社会实践项目;; 中国科学技术大学研究生创新基金
【CateGory Index】: P584
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