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9. 震旦系—南华系及其下伏地层物性分布统计直方图
(a)、(b)、(c)分别为震旦系—南华系的电阻率、密度和磁化强度分布；(d)、(e)、(f)为下伏地层对应的电阻率、密度和磁化强度分布
Fig.9. Statistical histogram of physical property distribution of Sinian-Nanhua system and its underlying strata
