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6. 不同充填程度暗河地质模型和正演成果地震剖面
a—正演地质模型;b—正演地震剖面
Fig.6. Geological model of underground river with different filling degree and seismic profile of forward modeling results
a—forward geological model;b—forward seismic profile
