传统的地震数据解释方法是利用地震剖面与水平切片的二维图象显示三维数据，它具有很大的局限性。
There exists great limitation on traditional seismic data interpretation method, which shows seismic data sets by displaying the planar image of seismic section and horizontal slice.
最后得到了冲绳海槽地区3d密度成像水平切片和2d密度成像剖面。
Finally, we get the 3d horizontal slice and the 2d profile of density imaging in the Okinawa Trough.
依据大量的地震剖面和水平切片等，分析火山岩的基本地震特征，并以此形成火山岩基本的识别模式。
Basis lots of the seismic profiles and level slice, analyse the fundamental seismic characteristics of the volcanic rocks, and thus formed the fundamental recognition mode of volcanics.
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