摘要
根据冲绳海槽多道地震资料的处理解释,在16条地震剖面上发现了水合物似海底反射层BSR,经过AVO、波形反演等特殊的处理技术,首次直接利用BSR圈定了冲绳海槽天然气水合物的具体分布范围,直接利用数据得出了天然气水合物稳定带厚度在冲绳海槽的分布趋势,认为海槽南部最厚,中部次之,北部最薄,并通过计算得出了冲绳海槽水合物稳定带的厚度和水合物资源量,对今后海槽水合物勘查和资源量评价具有一定的指导意义。
According to the processing and interpretation of multichannel seismic reflection data in the area of Okinawa Trough,the BSR（bottom simulating reflector） are identified in 16 seismic profiles. By special processing technology such as AVO and waveform inversions,the authors,for the first time,directly used BSR to outline the distribution extent of gas hydrate in the Okinawa Trough, used the data to know the distribution tendency of thickness of gas hydrate stability zone in the Trough and thought that the largest stability zone thickness was in the south and the smallest in the north. Then through calculation the authors got the thickness of hydrate stability zone and resources of the hydrate. This would be useful to the future hydrate explorations and resource evaluations in the Okinawa Trough.
出处
《海洋地质与第四纪地质》
CAS
CSCD
北大核心
2005年第4期79-84,共6页
Marine Geology & Quaternary Geology
基金
国家重点基础研究发展规划项目(G2000046703)
国家海洋局青年基金项目(2001509)
