轮古西地区奥陶系碳酸盐岩古暗河系统地震特征分析
但光箭1(
), 周成刚1, 刘云宏2, 李相文1, 张亮亮1, 张明1, 王春阳1
), 周成刚1, 刘云宏2, 李相文1, 张亮亮1, 张明1, 王春阳1
Seismic characteristics of the paleo-underground river system in Ordovician carbonate paleo-buried hills in the western Lungu area
DAN Guang-Jian1(), ZHOU Cheng-Gang1, LIU Yun-Hong2, LI Xiang-Wen1, ZHANG Liang-Liang1, ZHANG Ming1, WANG Chun-Yang1
), ZHOU Cheng-Gang1, LIU Yun-Hong2, LI Xiang-Wen1, ZHANG Liang-Liang1, ZHANG Ming1, WANG Chun-Yang1
图9. 轮古15井区暗河系统平面、剖面
a—LG15井区奥陶系潜山振幅属性平面;b—过主暗河地震剖面;c—过分支暗河地震剖面
Fig.9. Plan and section of underground river system in Lungu 15 well block
a—rms amplitude attribute map;b—seismic profile of the main underground river;c—seismic profile of the branches underground river
