面向起伏地表偏移成像的表层静校正方法

2012年 51卷 第No. 6期
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A new static correction method for the migration from rugged topography
同济大学海洋地质国家重点实验室,上海200092
Liu Yuzhu,State Key Laboratory of Marine Geology,Tongji University,Shanghai 200092,China
静校正量可以分为高频校正量与低频校正量。在缺乏精确的全深度速度模型的前提下,为了进行起伏地表偏
移成像,需要首先确定一平滑起伏基准面进行表层高频量校正,再进行自起伏基准面的速度分析与偏移成像。为此
,提出了基于层析模型的表层高频校正量提取方法及相应的平滑基准面确定方法。在理论模型与实际资料应用中与
传统方法进行了对比,证实了高频静校正与起伏基准面偏移成像相结合可以取得较好的效果。
Statics can be divided into low-frequency part and high-frequency part.On the premise of lacking accurate full-depth velocity,in
order to carry out migration from rugged topography,a smooth datum is needed to perform the high frequent static correction
prior to thevelocity analysis and migration.So,based on the tomography surface model,a new method to calculate the high
frequent statics and the corresponding smooth datum is proposed in this paper.Through comparing this new method with the
traditional methods on a synthetic data and a field data,we proved that high-frequency static correction following with
migration from the corresponding smooth datum achieves better result.
起伏地表; 静校正; 基准面; 层析成像; 偏移成像;
rugged topography; static correction; datum; tomography; migration;
10.3969/j.issn.1000-1441.2012.06.006