In:
Geochemistry, Geophysics, Geosystems, American Geophysical Union (AGU), Vol. 15, No. 6 ( 2014-06), p. 2180-2194
Kurzfassung:
Hydrocarbons (HC) at mud volcanoes (MVs) in the Kumano basin are thermogenic HCs most likely originate from the old accretionary prism deeper than 2300 m Except for MVs 2 and 5 seepage activity of MVs is low compared to former times
Materialart:
Online-Ressource
ISSN:
1525-2027
,
1525-2027
DOI:
10.1002/2013GC005057
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2014
ZDB Id:
2027201-7
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