Ming：More serious challenge in North China
After the Ming Dynasty moved its capital to Beijing, it faced even tougher challenges: being closer to the border, farther away from the Mother River, and falling into the earthquake zone. North China entered the 3rd period of high seismicity (1484— 1730). Seismicity in North China is constrained by...
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| Format: | Article |
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Editorial Office of Progress in Earthquake Sciences
2025-01-01
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| Series: | 地震科学进展 |
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| Online Access: | https://www.gjdzdt.cn/en/article/doi/10.19987/j.dzkxjz.2024-141 |
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| author | Rui Feng |
| author_facet | Rui Feng |
| author_sort | Rui Feng |
| collection | DOAJ |
| description | After the Ming Dynasty moved its capital to Beijing, it faced even tougher challenges: being closer to the border, farther away from the Mother River, and falling into the earthquake zone. North China entered the 3rd period of high seismicity (1484— 1730). Seismicity in North China is constrained by two active seismic belts: the NE-oriented Tangshan-Cixian belt and the NW-oriented Zhangjiakou-Penglai belt. The pair of conjugate fractures is cross-shear zones formed under the action of a uniform tectonic stress field with different orientations and opposite shear directions. The presence of conjugate fracture adds to the diversity of seismicity, and simulation experiments and field observations have investigated its mechanical mechanisms. The rupture networks in Eurasian continent also show the predominantly NE- and NW-oriented configuration, which can guide the analysis of stress transformation and earthquake precursors. |
| format | Article |
| id | doaj-art-f55c1c4228164409a9a93ed92a8439cc |
| institution | Kabale University |
| issn | 2096-7780 |
| language | zho |
| publishDate | 2025-01-01 |
| publisher | Editorial Office of Progress in Earthquake Sciences |
| record_format | Article |
| series | 地震科学进展 |
| spelling | doaj-art-f55c1c4228164409a9a93ed92a8439cc2025-01-07T06:13:58ZzhoEditorial Office of Progress in Earthquake Sciences地震科学进展2096-77802025-01-0155210812410.19987/j.dzkxjz.2024-1412024-141Ming：More serious challenge in North ChinaRui Feng0China Earthquake Networks Center, Beijing 100045, ChinaAfter the Ming Dynasty moved its capital to Beijing, it faced even tougher challenges: being closer to the border, farther away from the Mother River, and falling into the earthquake zone. North China entered the 3rd period of high seismicity (1484— 1730). Seismicity in North China is constrained by two active seismic belts: the NE-oriented Tangshan-Cixian belt and the NW-oriented Zhangjiakou-Penglai belt. The pair of conjugate fractures is cross-shear zones formed under the action of a uniform tectonic stress field with different orientations and opposite shear directions. The presence of conjugate fracture adds to the diversity of seismicity, and simulation experiments and field observations have investigated its mechanical mechanisms. The rupture networks in Eurasian continent also show the predominantly NE- and NW-oriented configuration, which can guide the analysis of stress transformation and earthquake precursors.https://www.gjdzdt.cn/en/article/doi/10.19987/j.dzkxjz.2024-141relocation of capital to beijingzhangjiakou-penglai seismic zoneconjugate fracturerupture network |
| spellingShingle | Rui Feng Ming：More serious challenge in North China 地震科学进展 relocation of capital to beijing zhangjiakou-penglai seismic zone conjugate fracture rupture network |
| title | Ming：More serious challenge in North China |
| title_full | Ming：More serious challenge in North China |
| title_fullStr | Ming：More serious challenge in North China |
| title_full_unstemmed | Ming：More serious challenge in North China |
| title_short | Ming：More serious challenge in North China |
| title_sort | ming more serious challenge in north china |
| topic | relocation of capital to beijing zhangjiakou-penglai seismic zone conjugate fracture rupture network |
| url | https://www.gjdzdt.cn/en/article/doi/10.19987/j.dzkxjz.2024-141 |
| work_keys_str_mv | AT ruifeng mingmoreseriouschallengeinnorthchina |