In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 17, No. 12 ( 2016-12), p. 4817-4835
Kurzfassung:
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
Materialart:
Online-Ressource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2016GC006643
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2016
ZDB Id:
2027201-7
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