Petrological and Metamorphic Evolution Study of the Staurolite-bearing Garnet Amphibolite in the Nyi

• 作 者: HUANG Jie ZHANG Cong YANG Jingsui CHEN Mei SHENG Tingting
• 机 构: State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of
• 出 处: Acta Geologica Sinica(English Edition)
• 发表日期: 2015年S2期
• 关键词: facies orogenic compositional garnet metamorphic variance typically experienced

1 Introduction Metamorphosed mafic rocks in orogenic belts usually involve high-variance assemblages which are stable very large regions of pressure(P)–temperature(T)and compositional(X)space.In particular,amphibolite facies mafic rocks typically contain similar assemblages:

1 Introduction Metamorphosed mafic rocks in orogenic belts usually involve high-variance assemblages which are stable very large regions of pressure (P) -temperature (T) and compositional (X) space. In particular, amphibolite facies mafic rocks contain similar assemblages: