哀牢山—红河断裂带中南段新生代构造活动的年代学证据

田鹏1, 杨周胜1, 喻聪骏2, 孙滨3. 2023. 哀牢山—红河断裂带中南段新生代构造活动的年代学证据. 中国地质调查, 10(2): 42-53. doi: 10.19388/j.zgdzdc.2023.02.06
引用本文: 田鹏1, 杨周胜1, 喻聪骏2, 孙滨3. 2023. 哀牢山—红河断裂带中南段新生代构造活动的年代学证据. 中国地质调查, 10(2): 42-53. doi: 10.19388/j.zgdzdc.2023.02.06
TIAN Peng, YANG Zhousheng, YU Congjun, SUN Bin. 2023. Chronological evidence of Cenozoic activity in the middle and southern part of Ailao Mountain-Red River fault zone. Geological Survey of China, 10(2): 42-53. doi: 10.19388/j.zgdzdc.2023.02.06
Citation: TIAN Peng, YANG Zhousheng, YU Congjun, SUN Bin. 2023. Chronological evidence of Cenozoic activity in the middle and southern part of Ailao Mountain-Red River fault zone. Geological Survey of China, 10(2): 42-53. doi: 10.19388/j.zgdzdc.2023.02.06

哀牢山—红河断裂带中南段新生代构造活动的年代学证据

  • 基金项目:

    云南省地震局青年基金项目“哀牢山—红河断裂带中段新生代活动性的年代学证据(编号: 2020K10)”和云南省重点研发计划(社会发展专项)“云南重大地震灾害及其灾害链综合风险评估技术与应用(编号: 202203AC100003)”联合资助

详细信息
    作者简介: 田鹏(1988—),女,工程师,主要从事地震地质研究工作。Email: 310235986@qq.com。
  • 中图分类号: P542;P533

Chronological evidence of Cenozoic activity in the middle and southern part of Ailao Mountain-Red River fault zone

  • 运用同位素年代学研究哀牢山—红河断裂带的构造演化历史已获得众多成果,但尚未有从低温—中温—高温系统的角度构建热演化史过程的研究,断裂带左旋走滑的启动时间仍存在争议。总结了哀牢山—红河断裂带中南段的年龄数据,通过分析认为相同同位素体系厘定的年龄值从南东端到北西端变新,差异性减小; 将研究区分为北、中、南3段,使用低温、中温、高温年龄构建时间-温度(T-t)变化曲线,热演化史表明断裂带经历了2期冷却历史,冷却速率和隆升剥蚀速率的时空变化记录了伸展应力自南向北依次传播、转换拉张强度在传递过程中逐渐减弱、断裂活动性明显减弱的过程; 将断裂带构造活动划分为快速左旋走滑阶段(35~20 Ma)、左旋走滑逐渐减弱阶段(20~ 6 Ma)及右旋走滑阶段(6 Ma至今)。断裂构造活动反映了印度—欧亚板块碰撞过程中,青藏高原东南缘的应力持续调节过程。
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收稿日期:  2022-05-17
修回日期:  2022-10-31
刊出日期:  2023-05-05

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