SEGMENTATION OF THE SHAOWU-HEYUAN FAULT ZONE AND THEIR ACTIVITY ASSESSMENT
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摘要: 邵武-河源断裂带是东南沿海地震亚区的西界。这条闽、赣、粤3省边界活动性断裂带包含3条形态各异、特征不同的较大断裂带,北段为邵武(福建)-石城断裂带,中段为瑞金-寻乌断裂带,南段为龙川(广东)-河源断裂带。3条断裂带并非首尾衔接,而是呈右列式多字型排列,长约750km,在江西境内近400km(占全长53%)。本文侧重研究江西境内的构造特征、地震、温泉和地裂缝展布特征,探讨其活动性以及对地壳稳定性的影响。笔者认为,邵武-河源活动性断裂带引起大震的可能性非常小,但分散小震有可能发生.Abstract: The Shaowu-Heyuan active fault zone bordering Fujian,Jiangxi and Guangdong Provinces,forms the west boundary of the sub-seismic zone of the southeast coastal area of China.It includes three sub-zones different in geometry and features.They are the northern Shaowu-Shicheng Fault Zone,the central Ruijing-Xunwu Fault Zone,and the southern Longchuan-Heyuan Fault Zone with a total length of about 750km.The three are not connected end to end,but en echelon arranged with the southern one overlapping successively the northern in a right manner.This article deals mainly with the activity of the part running through the Jiangxi Province in connection with the distribution of earthquakes,hot springs,and ground fissures and the effect on the stability of the earth's crust.The author comes to the conclusion that there is little possibility for a large earthquakes to occur along the Shaowu-Heyuan Fault Zone,though some scattered smaller ones not excepted.
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Key words:
- active fault zone /
- hot spring /
- earthquake /
- stress adjustment
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