In:
Journal of Geophysical Research: Solid Earth, American Geophysical Union (AGU), Vol. 124, No. 5 ( 2019-05), p. 4399-4427
Kurzfassung:
Free gas can migrate through the GHSZ if it is supplied in excess of the consumption by gas hydrate formation Effective gas transport through the GHSZ requires a high gas supply as it is possible in seismic pipe or chimney structures and faults Observed salinity peaks and temperatures are a result of intermittent high gas fluxes following overpressure buildup and fracturing
Materialart:
Online-Ressource
ISSN:
2169-9313
,
2169-9356
DOI:
10.1029/2019JB017417
Sprache:
Englisch
Verlag:
American Geophysical Union (AGU)
Publikationsdatum:
2019
ZDB Id:
2016813-5
ZDB Id:
161666-3
ZDB Id:
3094197-0
SSG:
16,13
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