The spatial distribution characteristics of Nb–Ta of mafic rocks in subduction zones
High field-strength elements have been regarded as one of the most important discriminations in subduction zone magma. However, the spatial distribution of Nb and Ta in subduction zone-related rocks has been rarely studied; it is still unclear whether there is a quantitative relationship between the...
Enregistré dans:
Auteurs principaux: | Li Weiwei, Ge Can, Wang Fangyue, Sun He, Gu Haiou |
---|---|
Format: | article |
Langue: | EN |
Publié: |
De Gruyter
2021
|
Sujets: | |
Accès en ligne: | https://doaj.org/article/302a1d2c243c4d1f9c77cba6e96100ae |
Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
Documents similaires
-
A Plate‐Mantle Convection System in the West Pacific Revealed by Tertiary Ultramafic‐Mafic Volcanic Rocks in Southeast China
par: Fa‐Bin Pan, et autres
Publié: (2021) -
Depth-dependent geometry of margin-parallel strike-slip faults within oblique subduction zones
par: Catalán,Nicole, et autres
Publié: (2017) -
Early Devonian Arc-Related Volcanic Rocks in the Haerdaban, North Margin of the Yili Block: Constraint on the Southward Subduction of the Junggar Ocean
par: Youxin Chen, et autres
Publié: (2021) -
Results in Geochemistry
Publié: (2021) -
Evidence of magma-water interaction during the 13,800 years BP explosive cycle of the Licán Ignimbrite, Villarrica volcano (southern Chile)
par: Lohmar,Silke, et autres
Publié: (2007)