Riphean Riftogenic Ophiolites and Conjugated Minerageny of the Southern Urals

摘要

The initial Early Riphean geodynamic environment of the Southern Urals and adjacent regions of the East European Platform was governed by the formation of a specific uplift of the Archean-Early Proterozoic crystalline basement with a rugged mountainous topography related to the ascent of an unconsolidated mantle diapir(Fig. la).