• 责任者：Gao Xiaoying (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) ; Li Shuning
• 刊名：Acta Petrologica Sinica
• 出版年：2011
• 卷期：27(2)
• 关键词：矿物包裹体 ; mineral inclusions ; 变质矿物 ; metamorphic minerals ; 超高压变质作用 ; ultrahigh pressure metamorphism
• 页码：p.469-489
• 图表：10 illus., 1 table, 130 refs.
• 分类号：0802
• issnNo：ISSN1000-0569
• isbnNo：CN11-1922/P

Ultrahigh-pressure (UHP) metamorphic rocks record the interactions between fluid/melt and rocks during the continental subduction and exhumation, presenting an excellent natural laboratory to study the composition and evolution of fluid/melt phases in deep subduction zones.  The multiphase solid (MS) inclusions enclosed in minerals of UHP metamorphic rocks provide the authors the key information on the behavior of fuild/melt during UHP metamorphism of continental crustal rocks. The occurrence of MS inclusions in UHP metamorphic rocks provides not only the important information on the composition and evolution of UHP metamorphic fluid/melt, but also insight into the metasomatism of fluid/melt at slab-arc depths. This paper presents an overview on the progress in the study of MS inclusions in UHP metamorphic rocks, with the emphasis on such outstanding issues as the formation mechanism, morphology and texture, mineral chemistry, trace element and fluid/melt origin.