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《Journal of Chengdu University of Technology(Science & Technology Edition)》 1982-03
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Geological Characteristics and Metamorphism of Nu Jiang Metamorphic Terrain, Eastern Tibet

Fu Gongqin;Pan Guitang;Xi Yuerong;Wang Peisheng  
The Nu Jiang metamorphic terrain in Eastern Tibet is one composed of theJia Yu Qiao group. It lies just on the turning point of the suture line of theGondwana plate and Eurasia plate. The Jia Yu Qiao group is analogous to theKhondalite series in the Condwana plate. Its metamorphic history may be roughly divided into two stages: the fisrtstage (Hercynian or earlier) was of regional metamorphism, which caused theJia Yu Qiao group to be changed into some schists and marbles of the green-schist facies; the second stage (Yanshan movement) produced the faulting zonesparallel to and defining the configuration of metamorphic terrain. The Jia YuQiao group underwent some dynamo-thermal metamorphism only in the faultingzones. During the Yanshan movement, when the Gondwana continental crustcollided against the Eurasia continental crust, no paired metamorphic beltswere produced. Only within the faulting zones of basement rocks, arepossible for dynamo-thermal metamorphism of higher pressure to occurs, i. e.the paired metamorphic belts are not necessary product of plate collision.
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