Mercury isotopic compositions of the Precambrian rocks and implications for tracing mercury cycling in Earth's interior
• Low Hg contents in metamorphic rocks support loss of Hg during metamorphism. • Similar Δ199Hg values between the equivalent un- and metamorphosed sedimentary rocks. • No significant Hg-MIF during the metamorphism. • Robust Hg-MIF signals for tracing the material cycling.
Gespeichert in:
| Autor*in: |
Deng, Changzhou [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2022 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: OC-043: Re-irradiation in head and neck cancers: A single institution prospective cohort study - Salunkhe, R. ELSEVIER, 2017, Amsterdam [u.a.] |
|---|---|
| Übergeordnetes Werk: |
volume:373 ; year:2022 ; day:1 ; month:06 ; pages:0 |
| Links: |
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| DOI / URN: |
10.1016/j.precamres.2022.106646 |
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Mercury isotopic compositions of the Precambrian rocks and implications for tracing mercury cycling in Earth's interior |
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• Low Hg contents in metamorphic rocks support loss of Hg during metamorphism. • Similar Δ199Hg values between the equivalent un- and metamorphosed sedimentary rocks. • No significant Hg-MIF during the metamorphism. • Robust Hg-MIF signals for tracing the material cycling. |
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• Low Hg contents in metamorphic rocks support loss of Hg during metamorphism. • Similar Δ199Hg values between the equivalent un- and metamorphosed sedimentary rocks. • No significant Hg-MIF during the metamorphism. • Robust Hg-MIF signals for tracing the material cycling. |
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• Low Hg contents in metamorphic rocks support loss of Hg during metamorphism. • Similar Δ199Hg values between the equivalent un- and metamorphosed sedimentary rocks. • No significant Hg-MIF during the metamorphism. • Robust Hg-MIF signals for tracing the material cycling. |
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