Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance.
Beijing plain is a strong earthquake tectonic area in China. There was a Sanhe-Pinggu earthquake with Ms8 that happened in1679. The seismogenic fault of this earthquake is called Xiadian fault. Our work found fault with a similar strike and opposite dip in the west of the Xiadian fault, which is cal...
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| Format: | Article |
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Public Library of Science (PLoS)
2022-01-01
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| Series: | PLoS ONE |
| Online Access: | https://doi.org/10.1371/journal.pone.0275436 |
| _version_ | 1797990777000820736 |
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| author | Jun Shen Xunye Dai Xuankai Jiao Bo Shao |
| author_facet | Jun Shen Xunye Dai Xuankai Jiao Bo Shao |
| author_sort | Jun Shen |
| collection | DOAJ |
| description | Beijing plain is a strong earthquake tectonic area in China. There was a Sanhe-Pinggu earthquake with Ms8 that happened in1679. The seismogenic fault of this earthquake is called Xiadian fault. Our work found fault with a similar strike and opposite dip in the west of the Xiadian fault, which is called the Xiadian west fault in this paper. Six shallow seismic profiles have been constructed to determine the location of the fault in Sanhe city, and the late Quaternary activity of the fault is studied with the method of combined drilling, magnetic susceptibility logging, and luminescence dating. The results of shallow seismic exploration show that the fault is zigzag and generally strikes NE and inclines NW. According to the core histogram and logging curves of ten boreholes and eight effective dating data, the buried depth of the upper breakpoint of the concealed fault is about 12 m, which dislocates the late Pleistocene strata. The effective dating result of this set of strata is 36.52 ±5.39 ka. The vertical slip rate has been about 0.075± 0.023 mm/a since the late Pleistocene and about 0.058 ± 0.030 mm/a since the late period of the late Pleistocene. It can be inferred that the Xiadian west fault is probably a part of the seismogenic structure of the Sanhe-Pinggu Ms8 earthquake that happened in 1679. In a broad sense, the Xiadian fault zone is likely to extend to the southwest along the Xiadian west fault. |
| first_indexed | 2024-04-11T08:41:46Z |
| format | Article |
| id | doaj.art-295dc3bbcb1f4a8387598fc2c65c0abd |
| institution | Directory Open Access Journal |
| issn | 1932-6203 |
| language | English |
| last_indexed | 2024-04-11T08:41:46Z |
| publishDate | 2022-01-01 |
| publisher | Public Library of Science (PLoS) |
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| series | PLoS ONE |
| spelling | doaj.art-295dc3bbcb1f4a8387598fc2c65c0abd2022-12-22T04:34:11ZengPublic Library of Science (PLoS)PLoS ONE1932-62032022-01-011710e027543610.1371/journal.pone.0275436Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance.Jun ShenXunye DaiXuankai JiaoBo ShaoBeijing plain is a strong earthquake tectonic area in China. There was a Sanhe-Pinggu earthquake with Ms8 that happened in1679. The seismogenic fault of this earthquake is called Xiadian fault. Our work found fault with a similar strike and opposite dip in the west of the Xiadian fault, which is called the Xiadian west fault in this paper. Six shallow seismic profiles have been constructed to determine the location of the fault in Sanhe city, and the late Quaternary activity of the fault is studied with the method of combined drilling, magnetic susceptibility logging, and luminescence dating. The results of shallow seismic exploration show that the fault is zigzag and generally strikes NE and inclines NW. According to the core histogram and logging curves of ten boreholes and eight effective dating data, the buried depth of the upper breakpoint of the concealed fault is about 12 m, which dislocates the late Pleistocene strata. The effective dating result of this set of strata is 36.52 ±5.39 ka. The vertical slip rate has been about 0.075± 0.023 mm/a since the late Pleistocene and about 0.058 ± 0.030 mm/a since the late period of the late Pleistocene. It can be inferred that the Xiadian west fault is probably a part of the seismogenic structure of the Sanhe-Pinggu Ms8 earthquake that happened in 1679. In a broad sense, the Xiadian fault zone is likely to extend to the southwest along the Xiadian west fault.https://doi.org/10.1371/journal.pone.0275436 |
| spellingShingle | Jun Shen Xunye Dai Xuankai Jiao Bo Shao Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance. PLoS ONE |
| title | Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance. |
| title_full | Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance. |
| title_fullStr | Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance. |
| title_full_unstemmed | Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance. |
| title_short | Late Quaternary activity of the Xiadian west concealed fault east to Beijing and its tectonic significance. |
| title_sort | late quaternary activity of the xiadian west concealed fault east to beijing and its tectonic significance |
| url | https://doi.org/10.1371/journal.pone.0275436 |
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