吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (4): 968-1004.doi: 10.13278/j.cnki.jjuese.201604102
李三忠1,2,3, 杨朝1,2, 赵淑娟1,2, 李玺瑶1,2, 索艳慧1,2, 郭玲莉1,2, 余珊1,2, 戴黎明1,2, 李少俊1,2, 牟墩玲1,2
Li Sanzhong1,2,3, Yang Zhao1,2, Zhao Shujuan1,2, Li Xiyao1,2, Suo Yanhui1,2, Guo Lingli1,2, Yu Shan1,2, Dai Liming1,2, Li Shaojun1,2, Mu Dunling1,2
摘要:
全球早古生代增生造山带极其发育,主要分布在古亚洲洋南北两侧、Iaeptus洋南侧、Rheic洋北侧和环冈瓦纳大陆地带,其中原特提斯洋封闭的产物主要发育在中国境内,大量微陆块在早古生代可能都是冈瓦纳北缘的俯冲-增生带中的重要组成。增生造山带中组成复杂,具有沟-弧-盆体系、海山、洋壳等残存记录,尤以榴辉岩发育为特征,增生造山成为早古生代古亚洲洋和特提斯洋构造体系的显著独特特征。早古生代末中亚早古生代造山带多为微陆块增生造山阶段,沟-弧-盆体系发育,具有增生-软碰撞造山的特点,发生时限较晚,为早古生代末; 原特提斯洋中的西昆仑、东昆仑、柴达木北缘、南阿尔金、北阿尔金与北祁连、北秦岭等围限或夹杂的微陆块在早古生代具有相同的增生造山过程,整体是向南俯冲线性增生到冈瓦纳大陆北缘,现今多次重复是早古生代弯山构造所致。400 Ma左右,南部古特提斯洋和北部勉略带的打开,导致其北漂,经复杂变形改造,它们现今为一巨型弯山构造横亘在中国中部,对中国构造格局影响最为重要。
中图分类号:
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