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三维勘探的解释者一定要利用数据体。从数据体得到的水平切片称为 Seiscrop~(TM)剖面,它具有独特的性质,根据它来作构造解释既快又方便,而且还有效。在 Seiscrop剖面上的同相轴显示出该处的走向,不需要作任何时间和空间校正,就能直接画出构造图等值线。在 Seiscrop 剖面上,同相轴的宽度由数据的频率和构造的倾角组成。同相轴终止表明在构造走向转换时,有断层或其它不连续现象。在单张 Seiscrop 剖面上平行于构造走向的断层是很不明显的,但是随着同相轴从一张剖面到另一张剖面作相对运动时,它就变得明显了。在实际成图时,通常在进到下一张之前,已画好一条断块的等值线,下一张与该张间的关系则由垂直剖面来
The interpreter of 3D exploration must use the data body. The horizontal slice from the body of data is called the Seiscrop ~ (TM) profile, which has unique properties from which it is quick and easy to interpret constructs and yet effective. The events on the Seiscrop profile show the direction of the formation and can be used directly to draw contour maps without any time and space corrections. On the Seiscrop section, the width of the events consists of the frequency of the data and the dip of the formation. The termination of the facies indicates the presence of faults or other discontinuities during the tectonic conversion. It is not obvious that the faults are parallel to the tectonic strike on a single Seiscrop profile, but it becomes apparent as the relative motion of a member from one profile to another. In the actual mapping, usually before moving on to the next one has drawn a broken contour, the next one with the relationship between the sheet by the vertical section to