When complex structure is encountered in magnetotelluric surveys, interpretation by locally fitted layered models is of questionable validity. However, when the processed data show two-dimensional structure, numerical inversion schemes for two-dimensional models may be constructed as an aid to regional data interpretation.
Wei‐Min LiuH. WangTao GuoMin YanZiyi Xi
Michael S. ZhdanovPatricia Pastana de LugãoOleg N. Portniaguine
Salah A. MehaneeMichael S. Zhdanov