采用射线追踪法的天然气水合物海底地震观测系统设计

摘要

Ray tracing method of basing on the subsurface geology model is very important for defining some parameters during marine seismic exploration. The signal reflected from underground interface can be directly viewed when different emission locations are chosen. Thus the effect of different seismic survey geometry on seismic data acquisition can be understood. It is also very significant for using multi-waves both to reveal the internal velocity structure of gas hydrates ores and enhance the resolution of gas hydrates bearing formations. By analyzing the application of ocean bottom seismometers (OBS) on the gas hydrate exploration abroad, the method of ray tracing was introduced on the layout design of OBS in this paper; PS wave was recorded in the sea test, which gives satisfied application result.%射线追踪法是以建立的地下地质模型为基础,研究不同的激发点发出的射线经地下地质界面反射后可以被接收到的信息,从而了解不同的观测系统对于特定地质条件地震资料采集的效果,对于海上地震采集相关参数的确定十分关键.在天然气水合物地震勘探中,丰富的多波勘探信息对于查清水合物内部速度结构、提高地层的分辨率具有重要意义.本文在分析国外天然气水合物海底地震仪(OBS,ocean bottom seismometer)勘探的应用成果基础上,采用射线追踪法理论计算和海上实验,实现了针对天然气水合物的海底地震观测系统设计,试验获得了转换横波记录,取得了良好的应用效果.