Birekte Terrane
The Birekte terrane is a terrane located by the Anabar Shield, in the north-eastern part of the Siberian Craton, in the basins of the Popigay, Anabar, Birekte and Olenyok rivers. It is defined entirely from geophysical data and is overlain by Riphean-Paleozoic platformal cover.[1][2][3][4][5][6]
References
[edit]- ^ van Kranendonk, Martin J.; Bennett, Vickie; Smithies, Hugh R.H. (eds.). Earth's Oldest Rocks. p. 827.
- ^ Condie, K.C. (ed.). Archean Crustal Evolution. p. 428.
- ^ Schematic map of the Siberian craton showing boundaries of the craton and its terranes[dead link]
- ^ Solov'Eva, L. V.; Kalashnikova, T. V.; Kostrovitsky, S. I.; Ivanov, A. V.; Matsuk, S. S.; Suvorova, L. F. (2017). "Phlogopite and phlogopite–amphibole parageneses in the lithospheric mantle of the Birekte terrane (Siberian craton)". Doklady Earth Sciences. 475 (1): 822–827. Bibcode:2017DokES.475..822S. doi:10.1134/S1028334X17070273.
- ^ Solov'Eva, L.V.; Kalashnikova, Т.V.; Kostrovitsky, S.I.; Ivanov, А.V.; Matsuk, S.S.; Suvorova, L.F. (2015). "Metasomatic and magmatic processes in the mantle lithosphere of the Birekte terrain of the Siberian craton and their effect on the lithosphere evolution". Geodynamics & Tectonophysics. 6 (3): 311–344. Bibcode:2015GeTec...6..311S. doi:10.5800/GT-2015-6-3-0184.
- ^ Altermann, Wladyslaw; Corcoran, Patricia (eds.). Precambrian Sedimentary Environments: A Modern Approach to Ancient Depositional Systems. p. 276.
External links
[edit] | This Russian Far East location article is a stub. You can help Wikipedia by expanding it. |