首页 | 本学科首页   官方微博 | 高级检索  
     检索      

天然气水合物层和游离气层的地震反演识别——布莱克海台USGS95-1测线应用实例
引用本文:李敏锋,刘学伟,白杰,童庆佳.天然气水合物层和游离气层的地震反演识别——布莱克海台USGS95-1测线应用实例[J].现代地质,2007,21(1):105-110.
作者姓名:李敏锋  刘学伟  白杰  童庆佳
作者单位:1. 中国地质大学"地下信息探测技术"教育部重点实验室,北京,100083;中国地质大学,地球物理与信息技术学院,北京,100083
2. 中国地质大学,地球物理与信息技术学院,北京,100083
基金项目:国家高技术研究计划发展专项经费;国家重点基础研究发展计划(973计划)
摘    要:利用基于弹性波阻抗的AVO反演方法对美国布莱克海台实际水合物存在区域的USGS95-1测线进行处理,得到了地震纵波波阻抗和横波波阻抗,并据此计算出泊松比和拉梅系数等弹性参数。对反演得到的各弹性参数分析发现:与同沉积的水饱和地层相比,含水合物的地层具有高的波阻抗和拉梅系数;而游离气层具有低的纵波波阻抗、泊松比和拉梅系数。据此推断出该测线上水合物层和游离气层的分布范围。认为波阻抗剖面和拉梅系数剖面上的近似平行于海底的高值带指示水合物层,且水合物层下伏所圈闭的低泊松比和低纵波波阻抗区域指示游离气的存在;还发现该条测线上的BSR主要是由其下的游离气的聚集引起。

关 键 词:弹性波阻抗  AVO  天然气水合物  泊松比  拉梅系数
文章编号:1000-8527(2007)01-0105-06
收稿时间:09 25 2006 12:00AM
修稿时间:12 15 2006 12:00AM

Identification of Gas-hydrate Sediments and Free Gas Layer Using Seismic Inversion Method: A Case Study of Line USGS95-1 in Blake Ridge
LI Min-feng,LIU Xue-wei,BAI Jie,TONG Qing-jia.Identification of Gas-hydrate Sediments and Free Gas Layer Using Seismic Inversion Method: A Case Study of Line USGS95-1 in Blake Ridge[J].Geoscience——Journal of Graduate School,China University of Geosciences,2007,21(1):105-110.
Authors:LI Min-feng  LIU Xue-wei  BAI Jie  TONG Qing-jia
Institution:1. Geo-detection Laboratory of Ministry of Education, China University of Geosciences, Bering 100083, China; 2. School of Geophysics and Technology Information, China University of Geasciences, Beijing 100083, China
Abstract:Compressional-wave impedance and shear-wave impedance of line USGS95-1 from Blake Ridge are obtained using elastic-impedance inversion method.Also,they are used to calculate Possion's ratio and Lame parameter of this line.All these elastic parameters are analyzed to identify the gashydrate sediments and free gas layer.The results show that the impedance and Lame parameter of the sediments containing gas hydrates are higher than those of the media with saturated water at the same depth,but for free gas layer,these two kinds of elastic parameters,with Possion's ratio,become very low.Therefore,the gas-hydrate area and free gas area can be outlined respectively according to these characteristics.The zone of paralleling bottom with high impedance and Lame parameter indicates the gas-hydrate layer,and the area with low impedance and Possion's ratio trapped by gas-hydrate layer below it symbolizes the accumulation of free gas.The analysis also shows the main factor that causes the BSR of this line is the free gas below it.
Keywords:AVO
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号