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冯锐. 南北朝·大地变迁的力源漫步地震五千年(8)[J]. 地震科学进展 . DOI: 10.19987/j.dzkxjz.2024-017
引用本文: 冯锐. 南北朝·大地变迁的力源漫步地震五千年(8)[J]. 地震科学进展 . DOI: 10.19987/j.dzkxjz.2024-017
Feng Rui. North-Southern Dynasties: Crustal stress fields[J]. Progress in Earthquake Sciences. DOI: 10.19987/j.dzkxjz.2024-017
Citation: Feng Rui. North-Southern Dynasties: Crustal stress fields[J]. Progress in Earthquake Sciences. DOI: 10.19987/j.dzkxjz.2024-017

南北朝·大地变迁的力源漫步地震五千年(8)

North-Southern Dynasties: Crustal stress fields

  • 摘要: 魏晋南北朝以来,佛教盛行,北方开凿了大量石窟,岩体的稳定性问题突显。地下应力场毕竟是地壳形变、岩体破坏、地震发生的直接力源,地学研究的基本课题。不久之前,通过大规模的国际合作使全球GPS速度场和地应力图完成更新,有了动力源的板块就不再是一堆僵化构造体,它们运动的活力和内部的应力状况被第一次揭示出来。本文介绍了地应力原地测量的方法,应力张量结构的划分原则,全球和中国应力图的基本特征。鉴于地震的震源机制解在构置应力图上的重要地位,作者绘制了多种三维透视图,便于读者以看图识字的方式掌握震源机制解的地质含义。最后,以两个实例对比了实测应力图和震源机制解的异同,分析了当地动力学的背景

     

    Abstract: Since the Wei, Jin, and North-Southern Dynasties, Buddhism has flourished and a large number of caves have been excavated in the northern China. Stability problems in rock stress fields highlighted. It is a direct source of force for crustal deformation, rock destruction, and earthquake occurrence. The update of the global GPS velocity field and World Stress Map was completed not long ago through large-scale international cooperation. Plates with the soul of a power source are no longer a bunch of rigid tectonics, and for the first time the dynamism of their movements and internal stresses are revealed. This paper describes the methods of in-situ measurement of stress, the principles of division of stress tensor regimes, and the basic features of stress maps. In response to the important position of earthquake focal mechanism in the constitutive stress map, the authors have drawn a variety of 3D perspective drawings, so that readers can easily grasp the geologic meaning of the earthquake focal mechanism in a way that is easy to read and understand by looking at the drawings. Finally, the background of the local dynamics is analyzed with two examples comparing the similarities and differences between the measured stress maps and the earthquake focal mechanism.

     

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