Its 3D seismic horizontal slices clearly display that each wave group appears such event ends as directional linear extension, the event image is dragged, the same event waveforms are apparently dislocated and suddenly changed, and a suit of waves is abruptly bended in a same direction.
走滑断层在三维地震水平切片上有清晰显示,主要表现为:各波组同相轴的终端呈线状定向延伸;波组同相轴图像有牵引现象;同属一套同相轴波组图形被明显错开;同相轴的波形突然变化;一套波组突然同向弯曲等。
Based on 3D seismic data body, it combines the interpretation technologies of binning slice, coherent body slice, horizontal slice, vertical section, bending section and inline slice to realize stereo spatial.
它从三维地震数据体出发,面块切片解释技术,相干体切片解释技术,水平切片解释技术,垂直剖面、弯曲剖面及沿层切片等技术的有机结合,实现立体空间解释,大大提高了构造及地质目的体解释的精度。
Sedimentary sandstone body of oxbow istracked and described using horizontal slice and 3D stereo display techniques, and its lithology is studied by analyzingreservoir depth, amplitude and frequency.
应用水平切片和三维立体显示技术对牛轭湖沉积砂岩体进行追踪和描述,利用储层厚度、振幅和频率分析方法研究其含油性。
By the use of 3D seismic data interpretation techniques, such as vertical time section time slice and surface slice.
利用三维地震资料解释技术,如垂直时间剖面水平切片及面块切片,根据其不同特征结合钻探资料,可以比较直观地判断岩浆侵入体的大小及范围。
