Can a 2-D MT frequency response always be interpreted as a 1-D response?

By Parker Robert L.  

Geophysical Journal International, Vol. 181, Iss. 1, 2010-04 ,pp. : 269-274

Oxford University Press

Access to resources Recommend Favorite

A simple 2-D explanation for negative phases in TE magnetotelluric data

By Selway K.   Thiel S.   Key K.  

Geophysical Journal International, Vol. 188, Iss. 3, 2012-03 ,pp. : 945-958

Oxford University Press

Access to resources Recommend Favorite

The 2-D magnetotelluric inverse problem solved with optimization

By Van Beusekom Ashley E.   Parker Robert L.   Bank Randolph E.   Gill Philip E.   Constable Steven  

Geophysical Journal International, Vol. 184, Iss. 2, 2011-02 ,pp. : 639-650

Oxford University Press

Access to resources Recommend Favorite

A nearly analytic symplectically partitioned Runge–Kutta method for 2-D seismic wave equations

By Ma Xiao   Yang Dinghui   Liu Faqi  

Geophysical Journal International, Vol. 187, Iss. 1, 2011-10 ,pp. : 480-496

Oxford University Press

Access to resources Recommend Favorite

Joint Inversion by means of Simulated Annealing in 2-D: II. The VLF Mode and Comparison with the VLF-R Results

By Kaikkonen P.   Sharma S.P.  

Physics and Chemistry of the Earth, Vol. 23, Iss. 9, 1998-01 ,pp. : 901-908

Elsevier

Access to resources Recommend Favorite