Geoelectromagnetic field of the Antarctic region by results of physical modeling

2011;
: 113-115
1
Carpathian Branch of the Institute of Geophysics NAS of Ukraine
2
Carpathian Branch of the Institute of Geophysics named after. SI. Subbotin NAS of Ukraine

The influence of surface conductive inhomogeneities on MT and MV soundings are analyzed by results of the physical modeling of geoelectromagnetic field of the Antarctic region. The 1D and 2D MT inversion results are compared.

  1. V.M. Kobzova, S.A. Deshchytsia, B.T. Ladanivskyi, I.P. Moroz. Fizychne modeliuvannia elektro­mahnitnykh poliv u heolohichnomu seredovyshchi. Kyiv. Naukova Dumka. 2008.
  2. R.G. Kurinin. Shema moshhnosti zemnoj kory Antarktidy. M:1:40000000
  3. Tektonicheskaja karta Antarktidy masshtaba 1: 10 000 000/Red. G. Je. Grikurov. M.: Kartfabrika ob#edinenija "Ajerogeologija" Mingeo SSSR, 1978
  4. M.P. Maslanyj, S.W. Garett, R.G.B. Renner,A.M. Smith Aeromagnetic Anomaly Map of West Antarctica (Wedell Sea Sector): Sheet 2 - BAS GEOMAP