The Sources of Cretaceous Magmatism in the Uda Sector of the Western Transbaikalian Rift Region Based on Geochemical and Isotopic (Sr, Nd, O, Pb) Data
Abstract The Uda, Yeravna, and Zaza riftogenic depressions belong to the Uda sector, which serves as the central fragment of the Western Trans-Baikal rift zone. New Sr–Nd–Pb–O isotopic data on the Cretaceous basaltic rocks from each depression in combination with geochemical data made it possible to estimate the compositions of mantle and crustal magmas and to propose a model for their mixing.
Authors
- E. N. Federyagina
- Д.А. Лыхин
- S. I. Dril
- С. А. Сасим
- A. A. Vorontsov
- V. M. Savatenkov
- V. V. Yarmolyuk
Institutions
- Institute of Geology of Ore Deposits Petrography Mineralogy and Geochemistry (RU)
- Vinogradov Institute of Geochemistry (RU)
- Institute of Precambrian Geology and Geochronology (RU)
- Irkutsk State University (RU)
Publication Details
- Journal
- Petrology
- Published
- 2026-07-22
- DOI
- https://doi.org/10.1134/s086959112670030x
- Primary Topic
- Geological and Geochemical Analysis
- Type
- article
- Field-Weighted Citation Impact
- 0.00