Granitoid Anorogenic Magmatism of the Yenisei Range: Evidence of Lithospheric Extension in the Western Part of the Siberian Craton
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DOI: 10.1134/s0016702920050055
Abstract: Abstract— Reproducing the geological evolution of the Yenisei Range is important not only to understand how mobile belts at boundaries between ancient cratons tectonically evolved but also to gain an insight into how the Siberian… read more here.
Keywords: siberian craton; evidence; yenisei range;