Pyroxenite melting at subduction zone: Implications for the origin of mafic arc magmas
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s11430-023-1118-3.pdf
Reference20 articles.
1. Borghini G, Fumagalli P, Rampone E. 2017. Partial melting of secondary pyroxenite at 1 and 1.5 GPa, and its role in upwelling heterogeneous mantle. Contrib Mineral Petrol, 172: 1–23
2. Bowman E E, Ducea M N. 2023. Pyroxenite melting at subduction zones. Geology, 51: 383–386
3. Chen L, Zhao Z F. 2017. Origin of continental arc andesites: The composition of source rocks is the key. J Asian Earth Sci, 145: 217–232
4. Chen L, Zhao Z F, Zheng Y F. 2014. Origin of andesitic rocks: Geochemical constraints from Mesozoic volcanics in the Luzong basin, South China. Lithos, 190–191: 220–239
5. Chen L, Zheng Y F, Xu Z, Zhao Z F. 2021. Generation of andesite through partial melting of basaltic metasomatites in the mantle wedge: Insight from quantitative study of Andean andesites. Geosci Front, 12: 101124
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1. Geochemical comparison between oceanic and continental arc volcanic rocks: Insights to arc magmatism;Geological Journal;2023-07-25
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