• 责任者：Shao Tongbin (Key laboratory of Isotope Geochemistry ; Guangzhou Institute of Geochemistry ; Chinese Academy of Sciences ; Guangzhou 510640 ; China) ; Ji Shaocheng
• 刊名：Geological Review
• 出版年：2011
• 卷期：57(6)
• 关键词：部分熔融 ; partial melting ; 流变学 ; rheology
• 页码：p.851-869
• 图表：16 illus., 168 refs.
• 分类号：0400
• 出版序号：20122225
• issnNo：ISSN0371-5736
• isbnNo：CN11-1952/P

This paper provides a state-of-the-art overview on the melt morphology and distribution in partially molten rocks under hydrostatic and dynamic conditions with special focuses on the influence of partial melting on rheological behavior of peridotite and granite. The presence of <5% melt results hence in only a modest rheological weakening due to the heterogeneous distribution of melt. With increasing the melt fraction, the partially molten rocks are significantly weakened, which leads to deformation-induced melt segregation or extraction.