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南海北部陆坡块体搬运沉积体系的地震响应与成因机制
引用本文:吴时国,秦志亮,王大伟,彭学超,王志君,姚根顺.南海北部陆坡块体搬运沉积体系的地震响应与成因机制[J].地球物理学报,2011,54(12):3184-3195.
作者姓名:吴时国  秦志亮  王大伟  彭学超  王志君  姚根顺
作者单位:1. 中国科学院海洋研究所,中国科学院海洋地质与环境重点实验室,青岛 266071; 2. 中国科学院研究生院,北京 100049; 3. 广州海洋地质调查局区域地质调查所,广州 510706; 4. 中海石油研究总院,北京 100027; 5. 中石油杭州地质研究院,杭州 310023
基金项目:国家重点基础研究计划(973计划),中国科学院重要方向性项目,国家自然科学基金
摘    要:块体搬运沉积体系是一种重力作用下形成的深水沉积体系,在全球大陆边缘沉积体系中扮演着重要角色.块体搬运沉积作用不仅造成危害极大的深水地质灾害,而且与海洋天然气水合物和深水油气的形成过程与富集有密切联系.根据新获得的海底地形地貌资料和地震资料,揭示了块体搬运沉积体系识别特征,明确了其分布范围.这些块体搬运沉积体系具有明显的...

关 键 词:块体搬运沉积体系  重力流  海底不稳定性  天然气水合物  海底滑坡  南海
收稿时间:2011-09-27

Seismic characteristics and triggering mechanism analysis of mass transport deposits in the northern continental slope of the South China Sea
WU Shi-Guo , QIN Zhi-Liang , WANG Da-Wei , PENG Xue-Chao , WANG Zhi-Jun , YAO Gen-Shun.Seismic characteristics and triggering mechanism analysis of mass transport deposits in the northern continental slope of the South China Sea[J].Chinese Journal of Geophysics,2011,54(12):3184-3195.
Authors:WU Shi-Guo  QIN Zhi-Liang  WANG Da-Wei  PENG Xue-Chao  WANG Zhi-Jun  YAO Gen-Shun
Institution:1. Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; 2. Graduate University, Chinese Academy of Sciences, Beijing 100049, China; 3. Institute of Geological Survey, Guangzhou Marine Geology Survey, Guangzhou 510706, China; 4. CNOOC General Research Institute, Beijing 100027, China; 5. Hangzhou Institute of Geology, PetroChina, Hangzhou 310023, China
Abstract:Mass transport deposits (MTDs) are one kind of deepwater sedimentary system driven by the gravity flow action, and play an important role in the deep-water sedimentation in the global continental margins. MTDs are not only one of the most serious deep-water geo-hazards, but also have close relationships with the formation and accumulation of marine gas hydrates and deepwater hydrocarbon. Based on the topographic and high resolution seismic data in the hydrocarbon exploration region, we reveal the discerned characteristics and distribution of the MTDs in the northern slope of the South China Sea. The MTDs are characterized by apparent geomorphology and sedimentary structures. The head of MTDs has well developed extensional fault; the middle of MTDs has slide and turnover block; in the toe region of MTDs occurred compressive structures and thrust faults. Several mechanisms can induce the development of MTDs. However, Baiyun MTDs were inferred to be dominated by the dissociation of gas hydrate after we have analyzed the model of gas hydrate reservoirs and numerical modeling by using elastic-plastic finite element method for the MTDs in the Baiyun sag. We calculated 6 sets of safety factors with 6 different dissociation levels of gas hydrate, and found that with the increasing dissociation of gas hydrate, the stability of submarine slope decreases.
Keywords:Mass transport deposits  Gravity flow  Seafloor instability  Gas hydrate  Submarine landslide  South China Sea
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