Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity

The Nanyuan–Tongxian fault is the boundary fault between the Beijing depression and the Daxing uplift, also the primary seismic-controlling fault of the Beijing M \begin{document}$ 6{\dfrac{1}{2}}$\end{document} earthquake in 1665. Its activity is of great significance to land planning and geologica...

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Main Authors: NIU Wenzhi, HE Fubing, LIU Zhenhua, CUI Yubin, BAI Lingyan, WANG Anguo, ZHANG Yueze, CAO Mengmeng, ZHOU Jieming
Format: Article
Language:zho
Published: Institute of Geomechanics, Chinese Academy of Geological Sciences 2023-12-01
Series:Dizhi lixue xuebao
Subjects:
Online Access:https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023032
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author NIU Wenzhi
HE Fubing
LIU Zhenhua
CUI Yubin
BAI Lingyan
WANG Anguo
ZHANG Yueze
CAO Mengmeng
ZHOU Jieming
author_facet NIU Wenzhi
HE Fubing
LIU Zhenhua
CUI Yubin
BAI Lingyan
WANG Anguo
ZHANG Yueze
CAO Mengmeng
ZHOU Jieming
author_sort NIU Wenzhi
collection DOAJ
description The Nanyuan–Tongxian fault is the boundary fault between the Beijing depression and the Daxing uplift, also the primary seismic-controlling fault of the Beijing M \begin{document}$ 6{\dfrac{1}{2}}$\end{document} earthquake in 1665. Its activity is of great significance to land planning and geological disaster prediction in Beijing. Using high-precision gravity, longitudinal-wave and shear-wave seismic comprehensive exploration profiles, and composite borehole geological profiles, this study investigated the geometric characteristics and activity of the northeastern section of the Nanyuan–Tongxian fault. The results show that after passing through Pingjiatuan Village in Tongzhou District, the fault turns to a nearly east-west direction, trending north with a dip angle of 56° to 75°. The new activity in the northeastern section exhibits characteristics of a normal fault, with an estimated buried depth of about 21.6 m, indicating it as a late Pleistocene active fault. The findings demonstrate that the activity age of the northeast section of the Nanyuan–Tongxian fault differs from that of the middle and southwestern sections, providing crucial geological foundations for the spatial planning and disaster reduction systems in the Beijing region.
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spelling doaj.art-45f49cd8201646a48a2ccb7fa108585f2024-01-18T06:53:29ZzhoInstitute of Geomechanics, Chinese Academy of Geological SciencesDizhi lixue xuebao1006-66162023-12-0129687988710.12090/j.issn.1006-6616.2023032Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activityNIU WenzhiHE FubingLIU Zhenhua0CUI YubinBAI LingyanWANG Anguo1ZHANG Yueze2CAO MengmengZHOU Jieming3Development and Research Center of China Geological Survey, Beijing 100037, ChinaBeijing Institute of Geological Survey, Beijing 100097, ChinaBeijing Institute of Geological Survey, Beijing 100097, ChinaBeijing Institute of Geological Survey, Beijing 100097, ChinaThe Nanyuan–Tongxian fault is the boundary fault between the Beijing depression and the Daxing uplift, also the primary seismic-controlling fault of the Beijing M \begin{document}$ 6{\dfrac{1}{2}}$\end{document} earthquake in 1665. Its activity is of great significance to land planning and geological disaster prediction in Beijing. Using high-precision gravity, longitudinal-wave and shear-wave seismic comprehensive exploration profiles, and composite borehole geological profiles, this study investigated the geometric characteristics and activity of the northeastern section of the Nanyuan–Tongxian fault. The results show that after passing through Pingjiatuan Village in Tongzhou District, the fault turns to a nearly east-west direction, trending north with a dip angle of 56° to 75°. The new activity in the northeastern section exhibits characteristics of a normal fault, with an estimated buried depth of about 21.6 m, indicating it as a late Pleistocene active fault. The findings demonstrate that the activity age of the northeast section of the Nanyuan–Tongxian fault differs from that of the middle and southwestern sections, providing crucial geological foundations for the spatial planning and disaster reduction systems in the Beijing region.https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023032quaternarynanyuan–tongxian faultcomposite drilling geological profile explorationcomprehensive geophysical profilesfault activity
spellingShingle NIU Wenzhi
HE Fubing
LIU Zhenhua
CUI Yubin
BAI Lingyan
WANG Anguo
ZHANG Yueze
CAO Mengmeng
ZHOU Jieming
Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity
Dizhi lixue xuebao
quaternary
nanyuan–tongxian fault
composite drilling geological profile exploration
comprehensive geophysical profiles
fault activity
title Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity
title_full Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity
title_fullStr Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity
title_full_unstemmed Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity
title_short Determination of the northeast section of the Nanyuan–Tongxian fault in Beijing and research on its Quaternary activity
title_sort determination of the northeast section of the nanyuan tongxian fault in beijing and research on its quaternary activity
topic quaternary
nanyuan–tongxian fault
composite drilling geological profile exploration
comprehensive geophysical profiles
fault activity
url https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023032
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