Trace element signature of subduction-zone fluids, melts and supercritical liquids at 120–180 km depth
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DOI: 10.1038/nature03971
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Cited by:
- Hong-Yan Li & Rui-Peng Zhao & Jie Li & Yoshihiko Tamura & Christopher Spencer & Robert J. Stern & Jeffrey G. Ryan & Yi-Gang Xu, 2021. "Molybdenum isotopes unmask slab dehydration and melting beneath the Mariana arc," Nature Communications, Nature, vol. 12(1), pages 1-10, December.
- Hong-Yan Li & Xiang Li & Jeffrey G. Ryan & Chao Zhang & Yi-Gang Xu, 2022. "Boron isotopes in boninites document rapid changes in slab inputs during subduction initiation," Nature Communications, Nature, vol. 13(1), pages 1-10, December.
- Xiaohui Li & Osamu Ishizuka & Robert J. Stern & Sanzhong Li & Zhiqing Lai & Ian Somerville & Yanhui Suo & Long Chen & Hongxia Yu, 2024. "A HIMU-like component in Mariana Convergent Margin magma sources during initial arc rifting revealed by melt inclusions," Nature Communications, Nature, vol. 15(1), pages 1-11, December.
- Yunchao Shu & Sune G. Nielsen & Veronique Roux & Gerhard Wörner & Jerzy Blusztajn & Maureen Auro, 2022. "Sources of dehydration fluids underneath the Kamchatka arc," Nature Communications, Nature, vol. 13(1), pages 1-14, December.
- Pitcher, Bradley W & Kent, Adam J.R., 2018. "Statistics and segmentation: Using Big Data to assess Cascades Arc compositional variability," Earth Arxiv 6xq3w, Center for Open Science.
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