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《长春地质学院学报》 1996-03
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Liu Xishan Liu Jianzhong Liu Xiang (Changchun University of Earth Sciences, Changchun 130026)  
For a long time, progressive and retrogressive metamorphisms have been divided into different phases of metamorphism developed under different environments or different stages of metamorphism during a single metamorphic cycle. The results presented here show that this classiffication is incorrect in some cases. The studies of geological setting, rock association, shear deformation fabric and chronology indicate that retrogressive metamorphism of archaean basement and progressive metamorphism of middle Proterozoic overlying sediment are the results of one metamorphism developing at the same time during the inter continental collision, which is called the double effect of metamorphism by this study and controlled by original rock feature, that is, crystallized or noncrystallized rocks. One example used to identify the metamorphic double effect is from the west part of Liaoning Province, where a napping battom base has been formed at 175-180 Ma. This napping battom base is composed of reworked complex of archaean crust and metamorphosed meddle proterozoic sedimentary rocks. Reworked complex includs mylonites, migmatized mylonites, migmatized mylonite gneisses and relict blocks of Archaean crust. Metamorphosed middle Proterozoic sedimentary rocks are composed of feldspar bearing quartzite, tremolite bearing marble and mica schist or phyllite (sometime containing graphite). It is specially pointed out that these metamorphosed sedimentary rocks are set in the archaean basement reworked complex as lensoid blocks. The mylonites and metamorphosed sedimentary rocks have the completely same feature in some respects, for example, the grade of retrogressive and progressive metamorphisms, shear deformation fabric and movement orientation as well as isotopic ages of muscovite ( 39 Ar- 40 Ar method). It is very clear that they are the products formed by one metamorphism at the same dynamothermal environment. It is reached that the recognition of the metamorphic doubl eeffect and its rock association is the key to understand evolutional model and crustal texture of intercontinental collision zone correctly.
【Fund】: 国家自然科学基金
【CateGory Index】: P588.3
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