精细井—震标定研究沉积层序旋回的方法
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摘要
为了解决沉积层序旋回的精细划分及在纵横向二维空间上的变化规律和横向延拓对比问题,本文提出利用小波深频分析方法,数值模拟出不同米氏周期旋回的单信号及复合信号,对模拟的多期复合信号再分解为单个频率旋回的单信号,并研发了井—震标定插入技术,实现了把单井频谱旋回特征标定到地震剖面中,进而搞清了频谱旋回在纵向、横向二维空间上的变化规律及展布特征,为确定区域沉积层序旋回的变化、地下地层结构及接触关系指明了方向。
To distinguishing sedimentary sequence cycles,and recognize two-dimensional space change law and lateral extension,this article develops a method for sedimentary sequence cycle research by well-seismic calibration.Using wavelet depth-frequency analysis,single signals and composite signals of different milankovitch cycles are obtained by numerical modeling.Then,the composite signals by numerical modeling can be broken down into single signals of singe frequency cycle.A developed well-seismic calibration insertion technology calibrates spectrum characteristics of singe frequency cycle from well data to seismic sections.The vertical-horizontal two-dimensional space changes and distribution characteristics of spectrum cycles are figured out,which help to recognize regional sedimentary sequence cycle variations,underground strata structure,and contact relationships.
引文
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