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Methane Seepage Caused by Gas Hydrate Dissociation in the Mid‐Okinawa Trough Since the Last Glacial Maximum

Abstract Submarine methane seepage can potentially be promoted by the dissociation of the marine hydrates surrounding the continental margins due to oceanic warming since the Last Glacial Maximum. This seepage could be archived by authigenic carbonates at seeping sites, but the time lag caused by he...

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Principais autores: Ang Li, Nengyou Wu, Qing Li, Zhou Wang, Yizhao Wan, Feng Cai, Zhilei Sun, Dong Feng
Formato: Artigo
Idioma:Inglês
Publicado em: Wiley 2023-06-01
coleção:Geophysical Research Letters
Assuntos:
cold seep
authigenic carbonate
uranium‐thorium dating
hydrate dissociation
Okinawa Trough
Acesso em linha:https://doi.org/10.1029/2023GL103375
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