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Spatially variable CO2 degassing in the Main Ethiopian Rift: Implications for magma storage, volatile transport and rift-related emissions

Abstract:

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 CO2 flux from the Eastern Rift of the East African Rift System (EARS) suggest this could equal emissions from the entire mid-ocean ridge system. We report new CO2 surveys from the Main Ethiopian Rift (MER, northernmost EARS), and reassess the rift-related CO2 flux. Since degassing in the MER is concen...

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Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1002/2017GC006975

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More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
More from this funder
Funding agency for:
Mather, T
Pyle, D
Grant:
NE/L013932/1
NE/L013932/1
A studentship as part of the Environmental Research DTP (University of Oxford
Publisher:
American Geophysical Union Publisher's website
Journal:
Geochemistry, Geophysics, Geosystems Journal website
Volume:
18
Issue:
10
Pages:
3714–3737
Publication date:
2017-10-30
Acceptance date:
2017-09-22
DOI:
ISSN:
1525-2027
Keywords:
Pubs id:
pubs:730575
UUID:
uuid:3879ee89-4186-42d8-8de6-3d6949107867
Local pid:
pubs:730575
Source identifiers:
730575
Deposit date:
2017-09-25

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