摘要
为得到水层反射所携带的水层速度信息,利用Munk公式描述水层速度的垂向变化,并在此基础上进行速度分析。通过引入水体地震记录同相轴补偿方法,在保留原始有效数据信息的同时,得到了与理论模型吻合的结果。将补偿及计算方法引入实际海洋反射地震的水体反射数据中,得到海水速度随反射时间的变化,为下一步的处理和成像提供了参考信息。
In order to obtain the water layer velocity information carried by the water layer reflection,Munk formula is used to describe the vertical change of the water layer velocity,and the velocity analysis is carried out on this basis.By introducing a compensation method for the events of the water body seismic record,while retaining the original effective data information,a result consistent with the theoretical model is obtained.The compensation and calculation methods are introduced into the water reflection data of actual ocean reflection seismic record.By this way,the change of sea water velocity with reflection time is obtained,which provides reference information for the next processing and imaging.
作者
高子傲
孙建国
GAO Zi'ao;SUN Jianguo(College of Geo-exploration Science and Technology,Jilin University,Changchun 130026,China)
出处
《世界地质》
CAS
2021年第4期924-934,944,共12页
World Geology
基金
国家重点研发计划(2019YFC0312004)。
关键词
声速剖面
Munk公式
水层反射
同相轴补偿
速度分析
sound velocity profile
Munk formula
water reflection
events compensation
velocity analysis