Structure and conditions of formation of the Tannuol intrusion (Tuva)
Authors:
Abstract
The Tannuol intrusion, one of the largest Lower Paleozoic granitoid intrusions of Tuva, which has a very complex petrographic composition and multiphase character of formation, was long considered as a plate-shaped body confined to the boundary of two lithologically and structurally different Cambrian and Ordovician formations, or as a folded flat-shaped body with steeply dipping wings in some folds. Structural and microstructural analysis of this intrusion has forced a reconsideration of the above notions.
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References
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