In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 18, No. 8 ( 2017-08), p. 2970-2989
Abstract:
We apply a systematic approach to quantify the rates of methane sources and sinks in different compartments in Taiwan accretionary prism CH4 production and consumption rates at shallow depth were nearly offset by each other, leaving total effluxes less than production at depth The potential flux imbalance could be likely accounted for by the sequestration of methane into hydrate forms and the clay absorption
Type of Medium:
Online Resource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2017GC006798
Language:
English
Publisher:
American Geophysical Union (AGU)
Publication Date:
2017
detail.hit.zdb_id:
2027201-7
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