| 摘要 |
<p>A method of three-component seismology wherein seismic energy induced vertical, radial and transverse particle movement is detected at plural spaced positions along a survey line to produce orthogonal data signals, and the different orthogonal data signals are variously processed both separately and interactively to develop novel signal relationships which improve indication and identification of steeply dipping reflections , out-of-plane reflections, and the like.</p> |
