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3. 塔里木盆地重磁电正演模型及其单一和联合反演结果
(a)电阻率正演模型；(b)密度正演模型；(c)磁化强度模型；(d)电阻率单一反演结果；(e)密度单一反演结果；(f)磁化强度单一反演结果；(g)电阻率联合反演结果；(h)密度联合反演结果；(i)磁化强度联合反演结果
Fig.3. Gravity-magnetic-magnetotelluric forward modeling，its single inversion results and joint inversion results in Tarim Basin
