La. Mastyulin et al., THE VERKHNEDVINSK GRABEN IS A NEW STRUCTU RE IN THE SYSTEM OF THE CENTRAL RUSSIAN AULACOGEN, Doklady Akademii nauk BSSR, 38(5), 1994, pp. 101-104
The paper present the results of magnetotelluric sounding in the north
ern part of Belarus. The Verchnedvinsk graben is distinguished within
the Kaunas-Polotsk deep fault zone and is the western segment of the C
entral Russian aulacogen. It was found to show the less tectonic activ
ity and smaller subsidence amplitude as compared to the other aulacoge
n structures.