Metamorphic Evolution and Anatexis of Gneissic Rocks in the Diancangshan-Ailaoshan Metamorphic Complex Belt, Southeastern Tibetan Plateau
详细信息
- 责任者：Wang Fang (State Key Laboratory of Continental Tectonics and Dynamics ; Institute of Geology ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Liu Fulai
- 刊名：Acta Petrologica Sinica
- 出版年：2011
- 卷期：27(11)
- 关键词：麻粒岩相 ; granulite facies ; 杂岩 ; complexes ; 深熔作用 ; anatexis ; 青藏高原 ; Qinghai-Tibetan Plateau
- 页码：p.3280-3294
- 图表：8 illus., 9 tables, 32 refs.
- 分类号：0802
- 出版序号：20122337
- issnNo：ISSN1000-0569
- isbnNo：CN11-1922/P
摘要
The gneissic rocks, which consist mainly of sillimanite-garnet-biotite gneiss, garnet biotite gneiss and staurolite-and kyanite-bearing sillimanite garnet gneiss, are widely distributed in the Diancangshan-Ailaoshan metamorphic complex belt. The results have an important significance for in-depth studying the metamorphic evolution, anatexis and dynamic process of the Diancangshan-Ailaoshan complex belt.