DOAJ Open Access 2022

Oxygen isotope (δ18O, Δ′17O) insights into continental mantle evolution since the Archean

Ilya N. Bindeman Dmitri A. Ionov Peter M. E. Tollan Alexander V. Golovin

Abstrak

The 18 O/16 O ratio of the subcontinental mantle has decreased by 0.2‰, while crustal values increased by 4‰ via fluid transfer since the Archean due to the initiation of plate tectonics and subduction, in line with the crust-upper mantle mass balance

Topik & Kata Kunci

Science

Penulis (4)

Ilya N. Bindeman

Dmitri A. Ionov

Peter M. E. Tollan

Alexander V. Golovin

Format Sitasi

APA MLA BibTeX

Bindeman, I.N., Ionov, D.A., Tollan, P.M.E., Golovin, A.V. (2022). Oxygen isotope (δ18O, Δ′17O) insights into continental mantle evolution since the Archean. https://doi.org/10.1038/s41467-022-31586-9

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Informasi Jurnal

Tahun Terbit: 2022
Sumber Database: DOAJ
DOI: 10.1038/s41467-022-31586-9
Akses: Open Access ✓