Glacigenic sedimentation pulses triggered post-glacial gas hydrate dissociation

Large amounts of methane are stored in continental margins as gas hydrates. They are stable under high pressure and low temperature, but react sensitively to environmental changes. Bottom water temperature and sea level changes were considered as main contributors to gas hydrate dynamics after the l...

Descripción completa

Detalles Bibliográficos
Autores principales: Karstens, Jens, Haflidason, Haflidi, Becker, Lukas W. M., Berndt, Christian, Rüpke, Lars, Planke, Sverre, Liebetrau, Volker, Schmidt, Mark, Mienert, Jürgen
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5809418/
https://www.ncbi.nlm.nih.gov/pubmed/29434195
http://dx.doi.org/10.1038/s41467-018-03043-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5809418/
https://www.ncbi.nlm.nih.gov/pubmed/29434195
http://dx.doi.org/10.1038/s41467-018-03043-z

Ejemplares similares