HR: 1330h
AN: T12A-0448 [PDF]
TI: TECTONIC FEATURES OF THE BARGUZIN DEPRESSION OF THE
BAIKAL RIFT ZONE USING COMPUTER INTERPRETATION OF ELECTRICAL
SOUNDINGS DATA
AU: * Nevedrova, N
EM: ninan@uiggm.nsc.ru
AF: Institute of Geophysics, Prospekt Koptyuga, 3, Novosibirsk, 630090
Russian Federation
AU: Epov, M
EM: mepov@uiggm.nsc.ru
AF: Institute of Geophysics, Prospekt Koptyuga, 3, Novosibirsk, 630090
Russian Federation
AU: Sanchaa, A
EM: aidisa@emf.ru
AF: Institute of Geophysics, Prospekt Koptyuga, 3, Novosibirsk, 630090
Russian Federation
AB:
In 1950s of the twentieth century, extensive geophysical prospecting was carried out
in the region of Baikal Rift Zone with the aim to investigate the deep depression structure.
The basic method of geophysical exploration was vertical electrical sounding (VES). At that
time, the sufficiently complicated structure of the section gave no way of determining the
main parameters of separate depositional sequences. With the development of computer
techniques it has become the possibility to interpret these complicated data of electrical
exploration at the new qualitative level by using programs of mathematical modelling and
inversion. At the first stage, interpretation of electrical prospecting data was executed based
on solution of the inverse problem within the limit of the horizontally-layered model using the
SONET program complex. Moreover, by using both 2D modelling and inversion, it is
possible to refine geoelectrical parameters and to conclude that entirely acceptable results can
be obtained using 1D inversion. The final results reflect the detailed deep depression
structure and it tectonic features. Tectonically active zone with multiple ruptures, which form
complicated block structures as in the sedimentary cover so in the base, are under
investigation.The sedimentary cover is as thick as 2.5 km according to results of computer
interpretation. Fractured zones exhibit the areas with decreased rock resistivity.
Reconstruction of a detailed tectonic structure of Barguzin depressions allow better
understanding peculiarities of geodynamic processes for the Baikal rift zone in general and for
depression in particular.
DE: 0910 Data processing
DE: 0925 Magnetic and electrical methods
DE: 8105 Continental margins and sedimentary basins
SC: Tectonophysics [T]
MN: 2003 Fall Meeting