耦合地震约束信息的重磁电联合反演方法及其应用——以塔里木盆地深层地质结构解析为例
杨敏1(
),于鹏2,朱光有1,张罗磊2,闫磊1,赵崇进2,马德波1,陈志勇1
),于鹏2,朱光有1,张罗磊2,闫磊1,赵崇进2,马德波1,陈志勇1
Gravity-magnetic-magnetotelluric joint inversion method coupled with seismic constraint information and its application： Case study of the analysis of deep geological structure in Tarim Basin
Min YANG1(),Peng YU2,Guangyou ZHU1,Luolei ZHANG2,Lei YAN1,Chongjin ZHAO2,Debo MA1,Zhiyong CHEN1
),Peng YU2,Guangyou ZHU1,Luolei ZHANG2,Lei YAN1,Chongjin ZHAO2,Debo MA1,Zhiyong CHEN1
图10. 联合反演9 km（a）和12 km（b）密度深度切片提取的断裂特征（图中黑色线条）
Fig.10. Fracture features extracted by joint inversion of density depth slices at 9 km(a) and 12 km(b) (black lines in the figure)
