Cargando…
Non-mantle-plume process caused the initial spreading of the South China Sea
The mantle plume process is thought to be the prevailing dynamic mechanism for the South China Sea opening, but controversy persists due to the lack of critical evidence of magma in the initial seafloor spreading. International Ocean Discovery Program (IODP) Expedition 367 successfully recovered at...
Autores principales: | Yu, Xun, Liu, Zhifei |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2020
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7244718/ https://www.ncbi.nlm.nih.gov/pubmed/32444825 http://dx.doi.org/10.1038/s41598-020-65174-y |
Ejemplares similares
-
Mantle heterogeneity caused by trapped water in the Southwest Basin of the South China Sea
por: Tian, Jinyu, et al.
Publicado: (2023) -
The evolution of the Galápagos mantle plume
por: Soderman, Caroline R., et al.
Publicado: (2023) -
Buoyant hydrous mantle plume from the mantle transition zone
por: Kuritani, Takeshi, et al.
Publicado: (2019) -
Martian magmatism from plume metasomatized mantle
por: Day, James M. D., et al.
Publicado: (2018) -
Low-buoyancy thermochemical plumes resolve controversy of classical mantle plume concept
por: Dannberg, Juliane, et al.
Publicado: (2015)