[1]张沛全,左天惠,邹 衍,等.右江断裂带旧州—泽屯小段的地貌与第四纪活动图像[J].华南地震,2024,(03):1-10.[doi:10.13512/j.hndz.2024.03.01]
 ZHANG Peiquan,ZUO Tianhui,ZOU Yan,et al.Geomorphology and Quaternary Activity Images of Jiuzhou-Zetun Sub Segment in Youjiang Fault Zone[J].,2024,(03):1-10.[doi:10.13512/j.hndz.2024.03.01]
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右江断裂带旧州—泽屯小段的地貌与第四纪活动图像()
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华南地震[ISSN:1006-6977/CN:61-1281/TN]

卷:
期数:
2024年03期
页码:
1-10
栏目:
地震科学研究
出版日期:
2024-09-30

文章信息/Info

Title:
Geomorphology and Quaternary Activity Images of Jiuzhou-Zetun Sub Segment in Youjiang Fault Zone
文章编号:
1001-8662(2024)03-0001-10
作者:
张沛全12左天惠3邹 衍3莫焱兰12杨会丽45
1.广西壮族自治区地震局,南宁 530022;2.广西壮族自治区震灾风险防治中心,南宁 530022;3.广西壮族自治区自然资源调查监测院,南宁 530201;4.地震动力学国家重点实验室,北京 100029;5.中国地震局地质研究所,北京 100029
Author(s):
ZHANG Peiquan12ZUO Tianhui3ZOU Yan3MO Yanlan12YANG Huili45
1.Earthquake Agency of Guangxi Zhuang Autonomous Region , Nanning 530022, China;2.Earthquake Risk Prevention Center of Guangxi Zhuang Autonomous Region , Nanning 530022, China;3.Natural Resources Survey and Monitoring Institute of Guangxi Zhuang Autonomous Region , Nanning 530201, China;4.State Key Laboratory of Seismic Dynamics , Beijing 100029, China;5.Institute of Geology , China Earthquake Administration , Beijing 100029, China
关键词:
右江断裂带构造地貌走滑断层里德尔剪切第四纪断层成熟度倾斜摄影测量
Keywords:
Youjiang River fault zone Tectonic geomorphology Strike-slip fault Riedel shear QuaternaryFault maturityOblique photogrammetry
分类号:
P931.1;P931.2;P546;P65;P231
DOI:
10.13512/j.hndz.2024.03.01
文献标志码:
A
摘要:
为探讨右江断裂带百色以西段北支旧州—泽屯小段的第四纪活动特征,从右江上游的乐里河、澄碧河流域的构造地貌研究入手,首先对两条河流开展遥感地质解译,利用河流地貌与断层活动的响应关系获取断层的可能部位,对断层活动可能出露的部位开展路线地质地貌调查并进行验证,试图勾勒出该小段断裂带的第四纪活动图像,最后讨论了该小段断裂带的第四纪活动的成熟度。遥感地质解译和野外调查的结果显示:旧州—泽屯小段断裂带的第四纪活动图像与构造物理实验中的R剪切断层发育阶段图像相似,其成熟度低。这可能是该小段断裂带至今缺乏5.0级以上的高震级地震记录的原因之一。
Abstract:
In order to explore the Quaternary activity characteristics of the Jiuzhou-Zetun sub segment in the northern branch of the western Baise section of the Youjiang fault zone, this paper first studied tectonic geomorphology of the Leli River and Chengbi River in the upper reaches of the Youjiang River. Firstly, remote sensing geological interpretation was carried out on the two rivers, and the response relationship between river geomorphology and fault activity was used to obtain the possible location of the fault. Geological and geomorphological surveys were conducted to verify the locations where fault zone activity may occur. The Quaternary activity images of the fault zone of the sub segment were sketched out. Finally, the maturity of the Quaternary activity of the fault zone was discussed. The results of remote sensing geological interpretation and field investigation show that the Quaternary activity images of the fault zone of the Jiuzhou-Zetun sub segment are similar to the images of the R shear fault in the development stage in tectonic physics experiments,and their maturity is low. This may be one of the reasons why there is still a lack of records about high magnitude earthquakes above 5.0 in this fault zone of the sub segment.

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备注/Memo

备注/Memo:
收稿日期:2024-05-21
基金项目:广西自然科学基金(2018GXNSFAA281323)
作者简介:张沛全(1978-),男,高级工程师,主要从事活动构造与构造地貌及相关工程应用工作。E-mail:zhangpeiquan2007@126.com
更新日期/Last Update: 2024-09-30