• 责任者：Ren Shenglian (School of Resources and Environmental Engineering ; Hefei University of Technology ; Hefei 230009 ; China) ; Song Chuanzhong
• 刊名：Geological Review
• 出版年：2011
• 卷期：57(6)
• 关键词：石榴子石族 ; garnet group ; 显微构造 ; ultrastructure ; 变质作用 ; metamorphism ; 片岩 ; schist ; 桐柏山 ; Tongbai Mountains
• 页码：p.799-809
• 图表：4 illus., 52 refs.
• 分类号：0802
• 出版序号：20122335
• issnNo：ISSN0371-5736
• isbnNo：CN11-1952/P

To study the metamorphic-deformation condition of rocks in ductile of shear zone is an important step to investigate the orogenic process and mechanism. Based on the study of characteristics of dislocations and the types of dynamic recrystallization of garnets in garnet-mica schists in Tongbai Mountains, east section of Shangdan fault (Shangnan-Danfeng fault) belt, the types of the plastic deformation, the deformation mechanism and the condition of deformation of garnets are identified. The garnets had been subjected to early medium-grade regional metamorphism, and then formed dislocations with high density and subgrains under the strong stress in the formation of shear zone, finally occurred plastic deformation.