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The origins and concentrations of water, carbon, nitrogen and noble gases on Earth
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“However, low N/C in today’s mid-ocean ridge source basalts (144) suggests considerable N2 degassing once the upper mantle became oxidized because then nitrogen became insoluble in magmas and upper mantle fluids (145).”
From The Archean atmosphere (2020) · cites this paper as [144]
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Metadata
- Authors
- Marty, B.
- Affiliations
- Centre National de la Recherche Scientifique (FR)
- Corresponding author
- Marty, Bernard
- ORCID
- Marty, Bernard
- Venue
- Earth and Planetary Science Letters
- Publisher
- Elsevier BV
- Published
- 2012-01
- Volume
- 313-314
- Pages
- 56-66
- ISSN
- 0012-821X (ISSN-L)
- OpenAlex
- W2095245998
- Cited by
- 1,012
- References
- 158
- Citations by year
- 2026: 50 · 2025: 71 · 2024: 87 · 2023: 70 · 2022: 81 · 2021: 79 · 2020: 90 · 2019: 70 · 2018: 93 · 2017: 75 · 2016: 62 · 2015: 69 · 2014: 48 · 2013: 39 · 2012: 23
- FWCI
- 19.04
- Type
- journal article
- Language
- en
- Open access
- green
- arxiv.org
- Locations
- Earth and Planetary Science Letters (publishedVersion)
- arXiv (Cornell University) (submittedVersion)
- HAL (submittedVersion, other-oa)
- arXiv (Cornell University)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Space and Planetary Science › Astro and Planetary Science
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geological and Geochemical Analysis
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Paleontology and Stratigraphy of Fossils
- Keywords
- water, carbon, nitrogen, noble gases, hydrogen isotopes, nitrogen isotopes, noble gas isotopes, primitive meteorites, cometary volatiles, radiogenic argon, carbonaceous chondrites, Earth accretion
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