A plate tectonic origin for Earth's hydrogen isotope dichotomy
The Earth's hydrogen isotope signature (D/H) is a primary tool for investigating the origins of terrestrial water and other volatiles. However, this signature is not uniform within the Earth. Whereas seawater D/H resembles that of carbonaceous chondri
Authors
- Amy L. Ferrick (ORCID: https://orcid.org/0000-0002-6547-8414)
- Jun Korenaga (ORCID: https://orcid.org/0000-0002-4785-2273)
Institutions
- Planetary Science Institute (US)
- Yale University (US)
Publication Details
- Published
- 2025-09-15
- DOI
- https://doi.org/10.22541/au.175795574.42955792/v1
- Primary Topic
- Methane Hydrates and Related Phenomena
- Type
- article
- Field-Weighted Citation Impact
- 0.00