Abstract

Paleotectonic reconstructions of the structural evolution of pre-Devonian sediments in the test area as geophysically-geologically indicated, including subsidence, uplift, warping, and other deformations, show in places, definite relationships between the pre-Devonian topography and the topography of the underlying crystalline base. Local variation in density, composition, and inner structures of the base may have its expression in the sedimentary topography and structure. — IGR Staff.

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