Could subduction-modified mantle explain high-<sup>186</sup>Os signatures in plume lavas?
- DOI
- 10.1016/j.scib.2026.05.074
- Published
- 2026-06-06
- Container
- Sci Bull (Beijing)
- Publisher
- Not recorded
- Open access
- no
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Cite this work
BibTeX
@article{allodium:10.1016/j.scib.2026.05.074,
title = {Could subduction-modified mantle explain high-\<sup\>186\</sup\>Os signatures in plume lavas?},
author = {Xu Y and Liu CZ.},
year = {2026},
journal = {Sci Bull (Beijing)},
doi = {10.1016/j.scib.2026.05.074},
url = {https://doi.org/10.1016/j.scib.2026.05.074}
}RIS
TY - JOUR TI - Could subduction-modified mantle explain high-<sup>186</sup>Os signatures in plume lavas? AU - Xu Y AU - Liu CZ. PY - 2026 JO - Sci Bull (Beijing) DO - 10.1016/j.scib.2026.05.074 UR - https://doi.org/10.1016/j.scib.2026.05.074 ER -
APA
Y, X., & CZ., L. (2026). Could subduction-modified mantle explain high-<sup>186</sup>Os signatures in plume lavas?. Sci Bull (Beijing). https://doi.org/10.1016/j.scib.2026.05.074
Source records
- europe-pmc · retrieved 2026-09-27T02:47:22.050Z