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...
محفوظ في:
| المؤلفون الرئيسيون: | , , , , , , , , |
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| التنسيق: | Artigo |
| اللغة: | Inglês |
| منشور في: |
Wiley
2024-04-01
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| سلاسل: | Geochemistry, Geophysics, Geosystems |
| الموضوعات: | |
| الوصول للمادة أونلاين: | https://doi.org/10.1029/2023GC011113 |
| الوسوم: |
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