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}}$\end{document} earthquake in 1665. Its activity is of great significance to land planning and geologica...
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Institute of Geomechanics, Chinese Academy of Geological Sciences
2023-12-01
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Series: | Dizhi lixue xuebao |
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Online Access: | https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023032 |
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author | NIU Wenzhi HE Fubing LIU Zhenhua CUI Yubin BAI Lingyan WANG Anguo ZHANG Yueze CAO Mengmeng ZHOU Jieming |
author_facet | NIU Wenzhi HE Fubing LIU Zhenhua CUI Yubin BAI Lingyan WANG Anguo ZHANG Yueze CAO Mengmeng ZHOU Jieming |
author_sort | NIU Wenzhi |
collection | DOAJ |
description | The Nanyuan–Tongxian fault is the boundary fault between the Beijing depression and the Daxing uplift, also the primary seismic-controlling fault of the Beijing M \begin{document}$ 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. |
first_indexed | 2024-03-08T13:16:12Z |
format | Article |
id | doaj.art-45f49cd8201646a48a2ccb7fa108585f |
institution | Directory Open Access Journal |
issn | 1006-6616 |
language | zho |
last_indexed | 2024-03-08T13:16:12Z |
publishDate | 2023-12-01 |
publisher | Institute of Geomechanics, Chinese Academy of Geological Sciences |
record_format | Article |
series | Dizhi lixue xuebao |
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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