Tracing Deep Carbon Cycling by Zinc Isotopes in a Peralkaline‐Carbonatite Suite
Abstract Sedimentary carbonates are known to be carried into the deep mantle by subducted slabs, and studies on mantle‐derived magmas have attempted to trace the recycled carbonate in their mantle source. However, the final depth of storage of recycled carbonate and the role of recycled carbonate in...
I tiakina i:
| Ngā kaituhi matua: | , , , , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Wiley
2024-04-01
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| Rangatū: | Geochemistry, Geophysics, Geosystems |
| Ngā marau: | |
| Urunga tuihono: | https://doi.org/10.1029/2023GC011113 |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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