海洋学研究 ›› 2013, Vol. 31 ›› Issue (1): 59-65.

• 研究论文 • 上一篇    下一篇

北黄海长山群岛外海底环状微洼地地貌特征

刘晓瑜1, 陈义兰1, 路波2, 文武2, 董立峰1   

  1. 1.国家海洋局 第一海洋研究所,山东 青岛 266061;
    2.国家海洋监测中心,辽宁 大连 116023
  • 收稿日期:2012-07-20 修回日期:2012-11-20 出版日期:2013-03-15 发布日期:2022-11-29
  • 作者简介:刘晓瑜(1982-),女,山西忻州市人,工程师,主要从事海底地形地貌和海洋工程地质方面的研究。E-mail:liuxiaoyu@fio.org.cn
  • 基金资助:
    国土资源部海洋区域地质调查资助项目(GZH200800501);国家海洋公益性行业科研专项经费资助项目(201005005)

Geographic features of the micro ring depreesions to the south of Changshan Archipelago at the north Yellow Sea

LIU Xiao-yu1, CHEN Yi-lan1, LU Bo2, WEN Wu2, DONG Li-feng1   

  1. 1. First Institute of Oceanography, SOA, Qingdao 266061, China;
    2. National Marine Environmental Monitoring Center, Dalian 116023, China
  • Received:2012-07-20 Revised:2012-11-20 Online:2013-03-15 Published:2022-11-29

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摘要： 得益于多波束测深系统对海底精细地形特征的展现能力,2011年在长山群岛南侧进行的多波束水深调查中一种特殊的环状微洼地地貌引起了调查人员的注意,该地貌形态与以往报道的海底侵蚀坑槽和洼地有很大的不同,且成群密集分布。本文依据多波束调查数据对环状微洼地的具体形态和地貌特征进行了详细描述,将环状微洼地分为3种不同的类型,并利用地形地貌分析手段,结合收集的地质环境资料对该地貌的成因进行探讨,认为该地貌形态应与海底浅层气体或油气泄漏有关,且后期受到水动力的改造。

关键词: 环状微洼地, 浅层气, 海底麻坑, 北黄海

Abstract: Benefit from the ability of displaying fine topography features of multi-beam sounding system, a special seabed landform drew much attention of the researchers during the investigation at the north Yellow Sea. This seabed landform was a kind of micro ring depression quite different from the submarine depressions reported previously. It developed at the plain seafloor in the water depth of 55 m to the south of the Changshan Archipelago, circular or irregular ellipse shape, with shallow grooves along the edge, protrusion or depression in the central. Each depression has different size, most of which has a major axis of about 2 km, with the shallow groove along the edge of 200~300 m wide and 0.25~2 m depth. Several micro depressions arranged in a row, with the regional trend of NW—SE or NE—SW.
The topography form and features of the micro ring depressions were described in detail in this paper based on the multi-beam survey data. They were divided it into three types with different distributions and morphologies. TypeⅠdistributed at the northeast of the area, circular or elliptical in plan view, with protrusion in the central. TypeⅡdistributed at the southeast of the area, to the north of TypeⅠarea, elliptical or elongated in plain view with depression in the central. Type Ⅲ distributed at the southwest of the area, curved in plain view, and much shorter and shallower than the previous ones. Given the circular or ellipse morphology, the annular micro depression may relate to the sub-bottom gas leakage, which can produce pockmarks with circular or elliptical shape. Meanwhile, shallow gas leakage produced by sub-bottom profile records and the deposit of peat discovered in boreholes 8 km south to the study area can support this opinion.
Therefore, it is possible that the micro ring depressions were formed by sub-bottom shallow gas leakage, and be transformed by bottom current and submarine slumping. If the suggestion can be confirmed, it will be great significance to the study of environmental evolution of the northern Yellow Sea and will provide new inspiration to the oil and gas exploration in this area.

Key words: ring depression, shallow gas, pockmark, the north Yellow Sea

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