Structure of Earth's crust in northeastern U.S.S.R.

Abstract
Recent geophysical studies of the Mesozoic geosynclinal region in northeastern U.S.S.R. show that the structure of the crust resembles most closely the Hercynian type. There have been almost no reconstructions of the crust until the most recent times. The neotectonics of the region is expressed by its barely significant and a really undifferentiated uplift. Activation is still too young to affect the position of the Mohorovičić boundary. - V.P. Sokoloff.

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