地震科学进展2025,Vol.55Issue(2) :108-124.DOI:10.19987/j.dzkxjz.2024-141

明·华北挑战更严峻——漫步地震五千年(13)

Ming:More serious challenge in North China

冯锐
地震科学进展2025,Vol.55Issue(2) :108-124.DOI:10.19987/j.dzkxjz.2024-141

明·华北挑战更严峻——漫步地震五千年(13)

Ming:More serious challenge in North China

冯锐1
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作者信息

  • 1. 中国地震台网中心,北京 100045
  • 折叠

摘要

明朝迁都北京后,面临的挑战更严峻:靠近了边境、离开了母亲河、掉进了地震带,对后世影响深远.华北地区进入第3次地震高发期(1484-1730).地震活动主要受制于两条活动地震带——NE向的唐山—磁县带和NW向的张家口—蓬莱带.这对共轭断裂形成于统一的构造应力场中,是一组走向不同、剪切方向相反的交叉剪切带.共轭断裂的存在,使地震活动的多样性更加突出,模拟实验和野外观测研究了它的力学机制.欧亚大陆的破裂网络也显示了以NE向和NW向为主的构架,对地震破裂的应力转化和前兆分析具有指导意义.

Abstract

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 trans formation and earthquake precursors.

关键词

迁都北京/张家口—蓬莱地震带/共轭断裂/破裂网络

Key words

relocation of capital to Beijing/Zhangjiakou-Penglai seismic zone/conjugate fracture/rupture network

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出版年

2025
地震科学进展

地震科学进展

ISSN:
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