北天山博乐盆地南缘勒塔干褶皱晚第四纪构造变形

胡宗凯; 李安; 原浩东; 苗树清; 杨晓平

doi:10.11899/zzfy20220101

北天山博乐盆地南缘勒塔干褶皱晚第四纪构造变形

doi: 10.11899/zzfy20220101

1.
地震动力学国家重点实验室, 中国地震局地质研究所, 北京 100029
2.
长安大学地质工程与测绘学院, 西安 050011

基金项目: 国家重点研发计划（2018YFC1504101）；国家自然科学基金面上项目（42072249）；中国地震局地质研究所基本科研业务专项（IGCEA1704）

详细信息

作者简介:
胡宗凯，男，生于1993年。博士。主要从事活动构造及地震地质研究工作。E-mail：zongkaihu2016@gmail.com

通讯作者:
杨晓平，男，生于1963年。博士生导师，研究员。主要从事活动构造及其地震危险性评价研究工作。E-mail：yangxiaoping-1@163.com

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出版历程
- 收稿日期: 2022-01-30
- 网络出版日期: 2022-05-31
- 刊出日期: 2022-03-31

Late Quaternary Tectonic Deformation of the Latgan Fold in the Southern Margin of the Bole Basin, North Tianshan

1.
State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
2.
College of Geological Engineering and Surveying of Chang'an University, Xi'an 710054, China

摘要

摘要: 研究天山地区活动逆冲断裂、褶皱对于认识整个天山再生造山带的隆升和地震危险性评估具有重要意义。以天山北麓博乐盆地南缘库松木楔克断裂东段勒塔干褶皱为研究对象，通过无人机航拍提取高精度DEM和野外实地调查结果，将勒塔干背斜东部迪里克河附近的洪积扇分为5期，从新到老分别为T1、T2、T3、T4、T5。其中，T4洪积扇完整记录了褶皱的变形历史，其后翼褶皱陡坎高度为（8.1±0.6）m。自T4洪积扇废弃以来，勒塔干断层的滑移量为（33.0±2.6）m。T3洪积扇仅发育在迪里克河出水口处，即勒塔干背斜北侧，（16.9±0.2）m的断层陡坎高度揭示了自T3洪积扇废弃以来，控制背斜形成的逆断层发生了21.4～21.7 m的滑动。通过与相邻地区洪积扇期次进行对比，认为T4洪积扇的废弃年龄为（74.01±6.14）ka，勒塔干背斜下断坡晚第四纪滑动速率为（0.45±0.05）mm/a，勒塔干褶皱晚第四纪地壳缩短速率为（0.37±0.04）mm/a。
- 活动褶皱 /
- 天山北麓 /
- 博乐盆地 /
- 勒塔干背斜 /
- 构造变形
Abstract: The study of active thrust faults and thrust folds in the Tianshan ranges is of great significance for understanding the uplift characteristic and earthquake hazard for the Tianshan. This paper focuses on the Latgan fold in the eastern segment of the Kusongmuxieke fault on the southern margin of the Bole Basin in the North Tianshan. Based on the high-precision DEM extracted by drone aerial photography and field surveys, we divided the alluvial fans which developed along the Dilik River in the eastern part of the Latgan fold into five generations, T1-T5 from young to old. The alluvial fan T4 completely records the deformation history of the fold. The height of the fold scarp of T4 is 8.1±0.6 m. Since the abandonment of the T4 alluvial fan, the dip-slip offset of the Latgan fault is 33.0±2.6 m. The T3 alluvial fan is only developed at the outlet of the Dilik River, that is, on the north side of the Latgan anticline. The 21.4-21.7 m dip-slip offset can be derived from the 16.9±0.2 m fault scarp since the T3 alluvial fan was abandoned. By comparing with the alluvial fan in adjacent areas, we can determine the abandoned ages of the T4 alluvial fan is 74.01±6.14 ka. Based on the lower dip-slip offset and T4 alluvial fan abandonment ages, the late Quaternary slip rate of the Latgan anticline and crustal shorting are 0.45±0.05 mm/a and 0.37±0.04 mm/a, respectively.
- Activity fold /
- Tianshan northern piedmont /
- Bole basin /
- Latgan anticline /
- Tectonic deformation

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图 1 天山地区活动构造

Figure 1. Active tectonics map in the Tianshan area

下载: 全尺寸图片幻灯片

图 2 博乐盆地和库松木楔克东段断层展布图

Figure 2. Fault distribution of Bole basin and eastern segment of Kusongmuxieke fault

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图 3 勒塔干背斜东段洪积扇分布

Figure 3. Alluvial fans distributions in the eastern segment of Latgan anticline

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图 4 勒塔干背斜及北翼逆断层

Figure 4. Lagtan anticline and thrust fault in the northern limb

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图 5 勒塔干褶皱东段地貌剖面图和断弯褶皱、铲状断层后翼抬升动力学模型图

Figure 5. Geomorphic profile of eastern segment of Latgan fold and back limb uplift dynamic model of fault-bend fold and listric fault

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图 6 勒塔干断层陡坎地形剖面图

Figure 6. Profile of the Latgan fault scarp

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