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6. 大地电磁TLE-3线重磁电联合反演结果
(a)大地电磁联合反演结果；(b)磁化强度联合反演结果；(c)密度联合反演结果（图中实线为泥盆系顶面、奥陶系顶面、寒武系顶面和寒武系底的已知地震约束，虚线为推断解释的震旦系—南华系底）
Fig. 6. Gravity-magnetic-magnetotelluric joint inversion result of magnetotelluric TLE-3 line
