Abstract
Numerous recently obtained geochronological data on the metamorphic and magmatic associations of the western part of the CAFB permitted distinguishing the Early Ordovician accretion-collision stage (490–450 Ma) in the development of this megastructure (Fig. 1).
Original language | English |
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Title of host publication | Geological Tour of Devonian and Ordovician Magmatism of Kuznetsk Alatau and Minusinsk Basin |
Publisher | Springer, Cham |
Chapter | 8 |
Pages | 191-213 |
Number of pages | 23 |
ISBN (Electronic) | 978-3-030-29559-2 |
ISBN (Print) | 978-3-030-29558-5 |
DOIs | |
Publication status | Published - 2020 |