Cargando…
Tiny droplets of ocean island basalts unveil Earth’s deep chlorine cycle
Fully characterising the exchange of volatile elements between the Earth’s interior and surface layers has been a longstanding challenge. Volatiles scavenged from seawater by hydrothermally altered oceanic crust have been transferred to the upper mantle during subduction of the oceanic crust, but wh...
Autores principales: | Hanyu, Takeshi, Shimizu, Kenji, Ushikubo, Takayuki, Kimura, Jun-Ichi, Chang, Qing, Hamada, Morihisa, Ito, Motoo, Iwamori, Hikaru, Ishikawa, Tsuyoshi |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6320363/ https://www.ncbi.nlm.nih.gov/pubmed/30610195 http://dx.doi.org/10.1038/s41467-018-07955-8 |
Ejemplares similares
-
Primitive noble gases sampled from ocean island basalts cannot be from the Earth’s core
por: Li, Yunguo, et al.
Publicado: (2022) -
Episodic entrainment of deep primordial mantle material into ocean island basalts
por: Williams, Curtis D., et al.
Publicado: (2015) -
Origin of ocean island basalts in the West African passive margin without mantle plume involvement
por: Belay, Iyasu Getachew, et al.
Publicado: (2019) -
Basaltic reservoirs in the Earth’s mantle transition zone
por: Tauzin, Benoit, et al.
Publicado: (2022) -
Deep microbial proliferation at the basalt interface in 33.5–104 million-year-old oceanic crust
por: Suzuki, Yohey, et al.
Publicado: (2020)