In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 17, No. 12 ( 2016-12), p. 4817-4835
Abstract:
Porewater geochemistry at the Takahe seep was linked to upward methane bubble transport and dissolution Modeling results showed that AOM and gas hydrate precipitation were the dominant processes in the methane cycle Model data were combined with geophysical data to constrain a seep‐wide methane budget
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2016GC006643
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2016
detail.hit.zdb_id:
2027201-7
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