Submit an Article
Become a reviewer
Vol 183
Pages:
242-245
Download volume:
RUS
Article

MODEM 3D new software for the interpretation of IP-affected 3D tem data

Authors:
M. I. Ivanov1
V. A. Kateshov2
I. A. Kremer3
M. I. Epov4
About authors
  • 1 — Engineer-programmer «RITM-Center»
  • 2 — Ph.D. General director «RITM-Center»
  • 3 — Engineer «RITM-Center»
  • 4 — Ph.D., Dr.Sci. Academician RAS, Director Institute of Oil and Gas Geology and Geophysics of Siberian Branch of Russian Academy of Sciences
Date submitted:
2008-10-26
Date accepted:
2008-12-14
Date published:
2009-12-11

Abstract

MODEM 3D software is presented, which is intended for direct modeling of formation processes of electromagnetic fields created by compound inductance-galvanic type sources (earthed horizontal electrical line) in time domain. Numerical stability of used algorithms is displayed on the example of medium, which contains nonstructural oil pool.

Область исследования:
Geophysics
Keywords:
3D modeling software inhomogeneous conducting medium induced polarization time domain
Go to volume 183

References

  1. Solution of 3D stationary Problems of DC Electrical Survey / M.I.Ivanov, V.A.Kateshov, I.A.Kremer, and M.V.Urev // Autometriya, 2007, N 2, V.43, pp.22-32.
  2. Solution of 3D-nonstationary TEM Problems / M.I.Ivanov, V.A.Kateshov, I.A.Kremer, and M.V.Urev // Autometriya, 2007, N 2, V.43, pp.33-44.

Similar articles

On specific features of stratigraphy of the middle devonian deposits of the Leningrad region
2009 M. G. Tsinkoburova
Comparative analysis of spiriferida complexes of the frasnian stage in the south of Novaya Zemlya and one-aged complexes of East-European platform and other districts
2009 D. V. Bezgodova
New data on infrared spectroscopy of diamonds from industrial deposits of Yakutia
2009 I. N. Bogush, S. I. Mityukhin, E. A. Vasiliev
Regularities of changes in strength of rocks under complicated stress state, different levels of humidity and pore pressure
2009 A. T. Karmansky
Thermobaric granite crystallization conditions of the severniy massif (the Chukotka) in accordance with the feldspars study data
2009 V. I. Alekseev
Analytical continuation of geophysical fields by continued fractions method
2009 K. M. Ermokhin