晋江龙湖湖盆古凹陷内古河流形成与消亡及与地震关系

徐起浩, 施建生. 晋江龙湖湖盆古凹陷内古河流形成与消亡及与地震关系[J]. 海洋地质与第四纪地质, 2012, 32(2): 53-63. doi: 10.3724/SP.J.1140.2012.02053
引用本文: 徐起浩, 施建生. 晋江龙湖湖盆古凹陷内古河流形成与消亡及与地震关系[J]. 海洋地质与第四纪地质, 2012, 32(2): 53-63. doi: 10.3724/SP.J.1140.2012.02053
XU Qihao, SHI Jiansheng. FORMATION AND ABANDONMENT OF A PALAEO-RIVER CHANNEL IN THE LONGHU LAKE DEPRESSION IN JINJIANG COUNTY, FUJIAN PROVINCE AND ITS RELATION TO PALAEO-EARTHQUAKE[J]. Marine Geology & Quaternary Geology, 2012, 32(2): 53-63. doi: 10.3724/SP.J.1140.2012.02053
Citation: XU Qihao, SHI Jiansheng. FORMATION AND ABANDONMENT OF A PALAEO-RIVER CHANNEL IN THE LONGHU LAKE DEPRESSION IN JINJIANG COUNTY, FUJIAN PROVINCE AND ITS RELATION TO PALAEO-EARTHQUAKE[J]. Marine Geology & Quaternary Geology, 2012, 32(2): 53-63. doi: 10.3724/SP.J.1140.2012.02053

晋江龙湖湖盆古凹陷内古河流形成与消亡及与地震关系

  • 基金项目:

    福建省晋江市人民政府与广东省地震局联合项目(2011)

详细信息
    作者简介: 徐起浩(1944-),男,研究员,从事地震地质学与海岸带第四纪地质学研究.E-mail:xuqihao2005@163.com
  • 中图分类号: P546

FORMATION AND ABANDONMENT OF A PALAEO-RIVER CHANNEL IN THE LONGHU LAKE DEPRESSION IN JINJIANG COUNTY, FUJIAN PROVINCE AND ITS RELATION TO PALAEO-EARTHQUAKE

  • 根据野外调查及龙湖湖内和沿岸共78个钻孔岩心揭示的龙湖及沿岸混合花岗岩及其风化土、残坡积层和晚更新世以来的沉积层展布,分析了龙湖成湖前的凹陷和发育在凹陷内的古河流环境。研究发现龙湖湖盆内下游古河床相对邻近上游河床被大幅度抬升达3 m余。龙湖的最早湖相沉积年龄为2 430±90 aBP,其年龄落在导致古森林更深沉没于海的深沪湾晚全新世强古地震的时间范围内,认为龙湖的形成可能与2 430 aBP左右深沪湾大地震,导致控制深沪湾陆地地堑的衙口-氵丙州断裂西北侧地块翘起掀升,使得湖盆凹陷内下游古河床被快速抬升,古河流被堵塞有关。龙湖是地震断塞湖,不同于断陷湖,是向斜坳陷湖的又一种构造湖。研究得出龙湖成湖前的古河流约在7 000 aBP开始形成,这正是导致深沪湾古森林首次沉没于海的深沪湾早全新世强古地震大致年龄,结合古河床形成前的凹陷形态,认为龙湖湖盆内古河流的形成可能与7 000 aBP左右深沪湾大地震导致龙湖地区环境改变有关。
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收稿日期:  2011-06-08
修回日期:  2011-08-23

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