The sources of Paleoproterozoic collisional granitoids (Sharyzhalgai uplift, southwestern Siberian craton) › Research Explorer

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The sources of Paleoproterozoic collisional granitoids (Sharyzhalgai uplift, southwestern Siberian craton): From lithospheric mantle to upper crust

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

DOI

https://doi.org/10.15372/RGG2019026
Final published version

O. M. Turkina
I. N. Kapitonov

Original language	English
Pages (from-to)	414-434
Number of pages	21
Journal	Russian Geology and Geophysics
Volume	60
Issue number	4
DOIs	https://doi.org/10.15372/RGG2019026
Publication status	Published - Apr 2019

Research areas

Collisional granitoids, Lu–Hf isotope composition, Mantle and crustal sources, Paleoproterozoic, Southwestern Siberian craton, Zircon, NORTHWESTERN PART, PROTEROZOIC POSTCOLLISIONAL GRANITOIDS, mantle and crustal sources, A-TYPE GRANITES, ROCKS, Lu-Hf isotope composition, DETRITAL ZIRCON, CONTINENTAL-CRUST, TRACE-ELEMENT, zircon, LU-HF ISOTOPE, U-PB AGE, SM-ND, southwestern Siberian craton, collisional granitoids

OECD FOS+WOS

ID: 20042110