Effect of water on seismic attenuation of the upper mantle: The origin of the sharp lithosphere–asthenosphere boundary

Oceanic lithosphere moves over a mechanically weak layer (asthenosphere) characterized by low seismic velocity and high attenuation. Near mid-ocean ridges, partial melting can produce such conditions because of the high-temperature geotherm. However, seismic observations have also shown a large and...

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Detalles Bibliográficos
Autores principales: Liu, Chao, Yoshino, Takashi, Yamazaki, Daisuke, Tsujino, Noriyoshi, Gomi, Hitoshi, Sakurai, Moe, Zhang, Youyue, Wang, Ran, Guan, Longli, Lau, Kayan, Tange, Yoshinori, Higo, Yuji
Formato: Online Artículo Texto
Lenguaje:English
Publicado: National Academy of Sciences 2023
Materias:
Physical Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10410724/
https://www.ncbi.nlm.nih.gov/pubmed/37523543
http://dx.doi.org/10.1073/pnas.2221770120

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10410724/
https://www.ncbi.nlm.nih.gov/pubmed/37523543
http://dx.doi.org/10.1073/pnas.2221770120

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