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跃进山岩系及其构造意义
引用本文:杨金中,邱海峻,孙加鹏,张兴洲.跃进山岩系及其构造意义[J].吉林大学学报(地球科学版),1998(4).
作者姓名:杨金中  邱海峻  孙加鹏  张兴洲
作者单位:中国科学院地质研究所,长春科技大学地球科学学院
摘    要:深入研究了跃进山岩系的物质组成与构造特点,确认其为佳木斯地体东缘晚古生代—中生代的增生杂岩,探讨了该杂岩形成与演化的构造作用过程。

关 键 词:跃进山岩系  跃进山地体  增生杂岩

YUEJINSHAN COMPLEX AND ITS TECTONIC SIGNIFICANCE
Yang Jinzhong.YUEJINSHAN COMPLEX AND ITS TECTONIC SIGNIFICANCE[J].Journal of Jilin Unviersity:Earth Science Edition,1998(4).
Authors:Yang Jinzhong
Abstract:s Yuejinshan complex is composed of weakly metamorphosed and strongly deformed rocks, granitoid and basic-ultrabasic rocks, which were originated from continental margin or island arc. Due to the high-pressure hornblendes and the jadeite, it is reasonable to be proposed that Yuejinshan complex had once experienced low temperature and high pressure metamorphism. The basic-ultrabasic rocks and Raohe ophiolites have been studied in detail, they are formed in different tectonic environment. Yuejinshan complex is the accretional complex which was formed during Yuejinshan terrane collision and accretion. According to the evolution history, a Mesozoic tectonic evolution model of the northeast Asia has been proposed, which includes following three stages: compressional subduction, extensional subduction and transform fault.
Keywords:Yuejinshan complex    Yuejinshan terrane    accretional complex
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