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Preliminary Study on Two Newly-Generated Seismotectonic Zones in North and Southwest China

机译:华北和西南两个新生代构造带的初步研究

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摘要

In previous seismotectonic studies, the emphasis was placed on the inherited active fault zones. In the recent tectonic stage that essentially keeps in step with the current regional geologic environment and the stress field, however, there are also some newly generated fault zones. By studying the seismicity in North and Southwest China, it has been known that the NE-trending Tangshan-Hejian-Cixian and NW-trending Tengchong-Gengma-Lancang seismic zones are just two newly generated fault zones. As distinguished from the inherited fault zones, they are called the newly generated seismotectonic zones. This paper deals with the existence of these two seismogenic zones from their seismicity and geological structures, gives a preliminary analysis of their characteristics, and shows their significance.
机译:在以前的地震构造研究中,重点放在继承的活动断层带上。然而,在最近的构造阶段,它基本上与当前的区域地质环境和应力场保持一致,但是,也有一些新产生的断层带。通过研究中国西北和西南地区的地震活动性,已经知道东北向的唐山-河间-磁县和西北向的腾冲-耿马-澜沧地震带只是两个新生成的断裂带。与继承的断裂带不同,它们被称为新生成的地震构造带。本文从地震和地质构造两个方面探讨了这两个成矿带的存在,对其特征进行了初步分析,并说明了它们的意义。

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