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舟山六横岛海域浅部地层结构 与水下滑坡分布特征
引用本文:孙鸿程,蔡廷禄,夏小明,王欣凯,刘毅飞.舟山六横岛海域浅部地层结构 与水下滑坡分布特征[J].海洋学研究,2019,37(1):59-66.
作者姓名:孙鸿程  蔡廷禄  夏小明  王欣凯  刘毅飞
作者单位:自然资源部 第二海洋研究所 国家海岛开发与管理研究中心,浙江 杭州,310012;自然资源部 第二海洋研究所 国家海岛开发与管理研究中心,浙江 杭州,310012;自然资源部 第二海洋研究所 国家海岛开发与管理研究中心,浙江 杭州,310012;自然资源部 第二海洋研究所 国家海岛开发与管理研究中心,浙江 杭州,310012;自然资源部 第二海洋研究所 国家海岛开发与管理研究中心,浙江 杭州,310012
基金项目:中央级公益性科研院所基本科研业务费专项项目资助(JG1205);国家自然科学基金面上项目资助(41576095)
摘    要:舟山群岛海域峡道密布,峡道边坡失稳现象普遍发育,规模不一。多发的水下滑坡对海底光缆、港口码头等海岸工程设施都有较大威胁。2012年12月,使用浅地层剖面仪对六横岛周边峡道区进行探测,划分出3个主要声学反射界面以及4个地层单元,上部3个地层为全新世沉积层。发现6处水下滑坡,分布于六横岛沿岸边坡及毗邻的潮流深槽边坡。滑坡结构均为整体性滑坡,部分具多级性。从滑坡体规模看,滑坡体体积介于1.6×105~2.7×107 m3之间,其中超大型滑坡2处、大型滑坡3处、中型滑坡1处。根据界面与滑坡体的相关性,推测水下滑坡均发生在距今2.5 ka以来的全新世晚期。

关 键 词:六横岛  峡道  浅部地层结构  水下滑坡
收稿时间:2018-09-29

Distribution characteristics of subaqueous landslides in the sea area of Liuheng Island,Zhoushan
SUN Hong-cheng,CAI Ting-lu,XIA Xiao-ming,WANG Xin-kai,LIU Yi-fei.Distribution characteristics of subaqueous landslides in the sea area of Liuheng Island,Zhoushan[J].Journal of Marine Sciences,2019,37(1):59-66.
Authors:SUN Hong-cheng  CAI Ting-lu  XIA Xiao-ming  WANG Xin-kai  LIU Yi-fei
Institution:State Research Center for Island Exploitation and Management,Second Institute of Oceanography, MNR, Hangzhou 310012, China
Abstract:The strait channels are densely covered in the sea area of Zhoushan Islands, and the instability of the slopes of the strait channels is generally developed and varied in scale. The frequent subaqueous landslides pose a greater threat to coastal engineering facilities such as submarine cables and port terminals. In December 2012, the sub-bottom profiles were detected in the sea area of Liuheng Island. Three main acoustic reflection interfaces and four formation units were divided, and the upper three formations were Holocene sedimentary layers. Six subaqueous landslides were found, which were scattered along the coast of Liuheng Island or adjacent to the strait channel slope. The landslides structure were whole landslide, and some of them were multi-step. From the scale of the subaqueous landslides, the volumes were between 1.6×105 to 2.7×107 m3, with 2 super-large landslides, 3 large landslides and 1 medium landslide. According to the correlation between the interface and the landslide body, it was speculated that the subaqueous landslides occurred in the late Holocene since 2.5 ka.
Keywords:Liuheng Island  strait channels  shallow stratum structure  subaqueous landslides  
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