绪言碳酸盐岩反演模型中包含着两个有意义的内容。一个是反演模型,即将地震道反演为“声阻抗测井”的形式,它是当前研究和发展的一种流行的方法;另一个内容则是碳酸盐岩,大家知道,碳酸盐岩油气储是众所瞩目的有开采效益的勘探对象。碳酸盐岩中常常存在着一些沉积建造,它本身的孔隙使得这些建造能够形成赋存烃类的圈闭。这些圈闭通常称之为礁或滩。礁块是一种生物岩礁,一般呈岗丘状或透镜状,并构成一种特殊的、错综复杂的地层圈闭。在许多情况下,地震资料,尤其是反演模型,具有检测这些对象的潜在能力。当 Introduction Carbonate inversion models contain two significant components. One is the inversion model, which is the inversion of seismic traces into the form of “acoustic impedance logging”, a popular method of current research and development; the other is carbonate rock, as we all know, carbonate Rock oil and gas storage is the focus of the exploratory exploration of mining benefits. There are often sedimentary deposits in carbonate rocks, whose own pores allow these constructions to form traps that carry hydrocarbons. These traps are often called reefs or beaches. Reef is a biological rock reef, usually hillock or lens-like, and constitute a special, intricate formation trap. In many cases, seismic data, especially inversion models, have the potential to detect these objects. when