The Physicochemical and Geodynamic Conditions of Formation of the Sarsangi Complex in the Boundary Zone between the Midd...
Published in Moscow University Geology Bulletin
Abstract—This article describes the geological structure of the Sarsangi gabbro–diorite–plagiogranite complex located in the boundary zone between the Middle and South Urals. The formation of its massifs took place in the Late Silurian in the abyssal zone at approximately 6.5–7.0 km. The temperature ranges of crystallization of granodiorites and ga...
