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The implications of H2S and H-2 kinetic stability in high-T mixtures of magmatic and atmospheric gases for the production of oxidized trace species (e.g., BrO and NOx)

Publication status:
Published

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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
More by this author
Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
Journal:
CHEMICAL GEOLOGY
Volume:
263
Issue:
1-4
Pages:
143-150
Publication date:
2009-06-15
DOI:
ISSN:
0009-2541
URN:
uuid:e3ec1243-3701-41fa-a71b-2019b7c80e4d
Source identifiers:
82967
Local pid:
pubs:82967

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