吉林大学学报(地球科学版) ›› 2016, Vol. 46 ›› Issue (4): 945-967.doi: 10.13278/j.cnki.jjuese.201604101
• 地质与资源 • 下一篇
李三忠1,2,3, 杨朝1,2, 赵淑娟1,2, 李玺瑶1,2, 郭玲莉1,2, 余珊1,2, 刘鑫1,2, 索艳慧1,2, 兰浩圆1,2
Li Sanzhong1,2,3, Yang Zhao1,2, Zhao Shujuan1,2, Li Xiyao1,2, Guo Lingli1,2, Yu Shan1,2, Liu Xin1,2, Suo Yanhui1,2, Lan Haoyuan1,2
摘要:
自新元古代罗迪尼亚超大陆裂解以来,早古生代是板块构造运动活跃时期,具有板块运动速度较快、构造格局不稳定、块体之间相互作用复杂多变等特征,造山带演化极其复杂,导致全球早古生代古大陆重建现今仍较模糊。特别是,早古生代末450~400 Ma存在全球性准同时的造山运动,已经出现俯冲增生、碰撞、陆内3种类型的全球尺度造山带。本文侧重论述全球早古生代碰撞类型造山带的特征,总结典型碰撞造山带最新的年代学、变质、变形和岩浆作用特征及其时空分布。早古生代全球碰撞型造山带主要分布在南半球的泛非造山带和北半球的加里东期造山带,分别与南方冈瓦纳大陆和北方劳俄古陆的初步集结密切相关,早古生代碰撞造山主要体现在大陆块之间的碰撞作用为特征。这些早古生代碰撞造山带具有近似的碰撞年龄,大致相同的演化过程。其中,南方大陆主体碰撞完成于540 Ma,而北方大陆主体集结完成于420 Ma,从全球构造意义上可能意味着全球一个420~400 Ma的超大陆初步形成。
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