Spatially variable CO2 degassing in the Main Ethiopian Rift: Implications for magma storage, volatile transport, and rift-related emissions
Deep carbon emissions from historically inactive volcanoes, hydrothermal, and tectonic structures are among the greatest unknowns in the long-term (∼Myr) carbon cycle. Recent estimates of diffuse CO2flux from the Eastern Rift of the East African Rift System (EARS) suggest this could equal emissions...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Published: |
Wiley
2017
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