西南三江地区新生代走滑造山

尹福光, 唐渊, 徐波. 2021. 西南三江地区新生代走滑造山. 沉积与特提斯地质, 41(1): 1-14. doi: 10.19826/j.cnki.1009-3850.2020.04001
引用本文: 尹福光, 唐渊, 徐波. 2021. 西南三江地区新生代走滑造山. 沉积与特提斯地质, 41(1): 1-14. doi: 10.19826/j.cnki.1009-3850.2020.04001
Yin Fuguang, Tang Yuan, Xu Bo. 2021. Cenozoic strike slip orogeny in Sanjiang area, Southwestern China. Sedimentary Geology and Tethyan Geology, 41(1): 1-14. doi: 10.19826/j.cnki.1009-3850.2020.04001
Citation: Yin Fuguang, Tang Yuan, Xu Bo. 2021. Cenozoic strike slip orogeny in Sanjiang area, Southwestern China. Sedimentary Geology and Tethyan Geology, 41(1): 1-14. doi: 10.19826/j.cnki.1009-3850.2020.04001

西南三江地区新生代走滑造山

  • 基金项目:

    全国陆域及海区地质图件更新与共享(成都地质调查中心) (DD20190375)

详细信息
    作者简介: 尹福光(1965—),男,研究员,主要从事区域地质矿产调查研究工作。E-mail:yfuguang@126.com
  • 中图分类号: P52

Cenozoic strike slip orogeny in Sanjiang area, Southwestern China

  • 本文系统论述了西南三江地区那邦、高黎贡山、崇山-澜沧江、点苍山-哀牢山-红河剪切走滑带、区域性伸展与变质核杂岩、新生代盆地及走滑过程中的碱性岩浆活动等特征,认为西南三江地区经历了挤压收缩变形(60~40Ma)、走滑伸展热隆(40~38Ma)、走滑剪切深熔(38~23Ma)、走滑剪切伸展(23~11Ma)、走滑剥蚀隆升(11~5Ma)5个时空演化阶段,并对应5种运动机制及动力学机制:碰撞挤压、走滑拉张热隆(岩浆)、走滑剪切深熔、剪切伸展、走滑垮塌,主要表现为走滑造山。西南三江造山带是印度板块向欧亚板块斜向俯冲形成的多条巨型顺时针走滑剪切带,其间的块体向南逸出并顺时针旋转。走滑断层系起了位移量调节和构造变换的作用,西南三江造山带为典型的走滑造山带。
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出版历程
收稿日期:  2020-04-03
修回日期:  2020-05-26

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