SEISMOLOGY AND GEOLOGY ›› 1995, Vol. 17 ›› Issue (4): 419-426.
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Zhang Hunan1, Ji Fengju2, Li Ziquan1, Chen Weiguang1, Liu Mingda2, Li Jianping2
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张虎男1, 计凤桔2, 李子权1, 陈伟光1, 刘明达2, 李建平2
基金资助:
地震科学联合基金(92090)
Abstract:
Based on the tectonic-geomorphic features,comparison of Quaternary system with isochron-ic geomorphic surface on both sides of the fault as well as the micro-and macro-structural indica-tions of the fault trace,the activity since late Pleistocene along the southern segment ofWuchuan-Sihui fault zone is discussed.It is suggested that this segment of the fault is relativelystable during this period.
Key words: Quantitative geomorphology, Fault activity’Thermoluminescent dating
摘要：
根据研究区的构造地貌特征,断裂两盘第四系和等时地貌面的对比以及其它宏观和微观的断裂构造迹象,讨论了四会-吴川断裂南段晚更新世以来的活动性,得出该时段、该断裂在该地区相对稳定的基本认识。
关键词: 定量地貌学, 断层活动性, 热释光法
Zhang Hunan, Ji Fengju, Li Ziquan, Chen Weiguang, Liu Mingda, Li Jianping. A STUDY ON THE RECENT ACTIVITY ALONG THE SOUTHERN SEGMENT OF WUCHUAN-SIHUI FAULT ZONE[J]. SEISMOLOGY AND GEOLOGY, 1995, 17(4): 419-426.
张虎男, 计凤桔, 李子权, 陈伟光, 刘明达, 李建平. 四会-吴川断裂南段近期活动性研究[J]. 地震地质, 1995, 17(4): 419-426.
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