• 责任者：Chen Renxu (Key Laboratory of Crust-Mantle Materials and Environments ; CAS ; School of Earth and Space Sciences ; University of Science and Technology of China ; Hefei 230026 ; China) ; Zheng Yongfei
• 刊名：Acta Petrologica Sinica
• 出版年：2011
• 卷期：27(2)
• 关键词：俯冲带 ; subduction zones ; 流体 ; fluids ; 变质矿物 ; metamorphic minerals ; 大别山 ; Dabie Mountains ; 苏鲁造山带 ; Su-Lu Orogenic Belt
• 页码：p.451-468
• 图表：9 illus., 182 refs.
• 分类号：0802
• issnNo：ISSN1000-0569
• isbnNo：CN11-1922/P

The Dabie-Sulu orogenic belt has been a type locality for the study of not only fluid regime but also chemical geodynamics in continental subduction zones. Hence the UHP metamorphic rocks from this belt are the main focus of this paper. Sources of metamorphic fluid can be deduced from study of hydrous minerals, structural hydroxyl and molecular water in nominally anhydrous minerals (NAMs). The decomposition of hydrous minerals and the exsolution of molecular water and structural hydroxyl during exhumation are responsible for the origin of retrograde fluid during exhumation of the deeply subducted continental crust.