U-Pb age of zircon from paragneisses in granulite terrane of the Sharyzhalgai uplift (southwest of the Siberian craton) › Research Explorer

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U-Pb age of zircon from paragneisses in granulite terrane of the Sharyzhalgai uplift (southwest of the Siberian craton): Evidence for the Archean sedimentation and evolution of continental crust from Eoarchean to Mesoarchean

Research output: Contribution to journal › Article › peer-review

Laboratory for the Evolution of Paleoocean and Mantle Magmatism

DOI

https://doi.org/10.1016/j.rgg.2016.07.007
Final published version

O. M. Turkina
S. A. Sergeev
V. P. Sukhorukov
N. V. Rodionov

Original language	English
Pages (from-to)	1018-1031
Number of pages	14
Journal	Russian Geology and Geophysics
Volume	58
Issue number	9
DOIs	https://doi.org/10.1016/j.rgg.2016.07.007
Publication status	Published - 1 Sept 2017

Research areas

Archean, detrital zircon, paragneisses, sedimentation, Sharyzhalgai uplift, SHRIMP, U-Pb age, METAMORPHIC EVENTS, METASEDIMENTARY ROCKS, DETRITAL ZIRCON, GNEISS BLOCK, PALEOPROTEROZOIC AGE, LU-HF ISOTOPE, IRKUT BLOCK, METATERRIGENOUS ROCKS, PLATFORM BASEMENT, SILLIMANITE SCHIST DEPOSIT

OECD FOS+WOS

ID: 9890564