Conjugation with the Central Asian Foldbelt: Interpretation of the 3dv and Tynda-Amurzet Transects
In this paper we consider the results of geological interpretation of 3DV (Tommot-Skovorodino segment) and Tynda-Amurzet geophysical transects crosscutting the Aldan Shield and the Stanovoi Granite-Greenstone Domain of the Siberian Platform; the Selengino-Stanovoi, Mongolia-Okhotsk, and Gobi-Hinggang foldbelts; and the Argun and Mamyn microcontinents with a total extent of sections of about 1000 km and depth of about 40 km. The data of previous studies and follow-up electric conductivity information have been used. The data of geological mapping, subject studies, and insights into the deep-seated structure of the considered territory obtained with a complex of geophysical methods are discussed. It is shown that Mesozoic strikeslip and thrust faults play the leading role in the present-day structure of the territory and in control rifting and mantle diapirism. It is suggested that Californian-type metamorphic nuclei, which are of structure-forming significance for adjacent territories in the west, have also developed in the studied region.