摘要
以三维高分辨地震与海底高频地震仪(OBS)联合勘探数据为基础,获得海底之下沉积层的地震反射成像剖面及多波信息,并以此确定研究区含天然气水合物沉积层的纵、横波速度的变化特征.根据走时反演获得的横波速度与纵波速度对比分析发现,研究区海底之下500m深度范围内的某些沉积层具有较高的纵横波速度,这一纵波速度升高区域与水合物稳定带对应,而纵波速度下降并且横波速度变化较小的区域,可能与游离气的存在相关.游离气的可能存在与基于这一区域2007年钻探测井结果的普遍认识不完全相符.
Based on integrated data acquired with 3-D seismic survey and OBS, both the images of subsurface formation and the information of P/S-wave velocities are obtained, which help to make certain the variation of P/S-wave velocity within the gas-hydrate bearing sediments in the study area. Comparison with the results of P/S-wave velocity calculated from travel time inversion indicates that some sediments have relatively high P/S-wave velocity within the depth of 500 m below seafloor. The abrupt rising of P-wave velocity means the presence of gas hydrate and the high velocity interval corresponds to the hydrate stable zone apparently, but the P-wave velocity decreasing as well slight S-wave velocity decreasing is very likely related to the occurrence of free gas. The presumed occurrence of free gas in the area does not agree with the viewpoints deduced from drilling and coring results within limited depth in this area in 2007.
出处
《地球物理学报》
SCIE
EI
CAS
CSCD
北大核心
2014年第4期1169-1176,共8页
Chinese Journal of Geophysics
基金
国际科技合作项目(2010DFA21630-2)
国家重点基础研究发展计划(973计划)(2009CB219)
国家青年科技基金(41206047)联合资助
关键词
神狐海域
联合勘探
OBS
天然气水合物
声波速度
Shenhu Area
Integrated exploration
Ocean bottom seismometer
Gas hydrates
Acoustic velocity
