In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 19, No. 11 ( 2018-11), p. 4476-4486
Abstract:
Mantle‐derived helium detected in cold methane seeps at the Cascadia Margin can be used as tracer for deep fracture systems Multiple methane sources as well as mixing and oxidation processes are present at the Cascadia Margin cold seeps The Cascadia Margin seeps are unequivocally dominated by methane
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1029/2018GC007859
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2018
detail.hit.zdb_id:
2027201-7
Permalink