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龙海流会—漳浦将军澳断裂活动与地震
引用本文:黄卿团,庄进耀,谢志招,张清香.龙海流会—漳浦将军澳断裂活动与地震[J].福建地震,2004(4).
作者姓名:黄卿团  庄进耀  谢志招  张清香
作者单位:厦门地震勘测研究中心 (黄卿团,庄进耀,谢志招),厦门地震勘测研究中心(张清香)
摘    要:福建龙海流会 -漳浦将军澳断裂展布于九龙江口以南沿海 ,地质构造上属于长乐—诏安断裂带南段 ,是我国东南沿海晚第三纪玄武岩喷发的地区之一。本文分析了龙海流会 -漳浦将军澳断裂从晚第三纪 -第四纪晚更新世多次的玄武岩喷发及活动特征 ,探讨了活动断裂与地震的关系 ,分析了地质旅游综合开发的潜在优势。研究结果表明 :龙海流会 -漳浦将军澳断裂是晚第三纪 -第四纪晚更新世早期 (N2 -Q3)玄武岩循其多次喷发 ,晚更新世 (Q3)活动明显 ,属晚更新世活动断裂 ;该断裂附近今后仍有可能发生 5级左右地震 ,应加强地震监测 ;本区玄武岩火山口及名胜古迹旅游资源十分丰富 ,可努力使其成为今后发展的重要行业。

关 键 词:龙海-漳浦沿海  断裂活动  地震

Active Fault and Earthquake along sea in LiuHei of LongHai to JianJunAo of ZhangPu
Huang Qingtuan,Zhuang Jinyao,Xie Zhizhao,Zhang Qingxiang.Active Fault and Earthquake along sea in LiuHei of LongHai to JianJunAo of ZhangPu[J].Fujian Seismology,2004(4).
Authors:Huang Qingtuan  Zhuang Jinyao  Xie Zhizhao  Zhang Qingxiang
Institution:Xiamen Center fot earthquke Prospecting and Researching
Abstract:LongHai to ZhangPu that is at the south section fault from ChangLe to ZhaoAn where break forth tht basalt at latest teriary and quaternary for LiuHuei in LongHai to JiangJunOu in ZhangPU that is the south area for the riverfor JiuLongJian. The paper is analysed the active character of the fault from the last-quaternary and the combinatorial charcter of the fault from the latest quaternary and the combinatorial charcter, the charcter that the basalt was break forth along the fault from the latest tertiary to quaternary,it discusses the relation fo active obviously at the latest Pleistocene,the basalt was break forth along the fault from the latest tertiary to the latest quaternary(N2-Q3),it is obviously active from the quaternary. It shall happening the earthquake of 5 grade in the future. We must enhance the seismic inspect. The resource of tour is enough, it will develop in the future.
Keywords:Along sea of Longhai to ZhangPU  active fault  earthquake
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