Compositional evolution of slab-derived fluids during ascent: implications from trace-element partition between hydrous melts and Cl-free or Cl-rich aqueous fluids-Reference-Cited by-同舟云学术

Compositional evolution of slab-derived fluids during ascent: implications from trace-element partition between hydrous melts and Cl-free or Cl-rich aqueous fluids

Published:2024-04-26 Issue:5 Volume:179 Page:
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contrib Mineral Petrol

Author:

Taniuchi Hajime^ORCID,Kawamoto Tatsuhiko,Nakatani Takayuki,Ishizuka Osamu,Suzuki Toshihiro,Tomiya Akihiko

Funder

Japan Society for the Promotion of Science

Publisher

Springer Science and Business Media LLC

Link

https://link.springer.com/content/pdf/10.1007/s00410-024-02122-3.pdf

Reference77 articles.

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2. Allabar A, Nowak M (2018) Message in a bottle: Spontaneous phase separation of hydrous Vesuvius melt even at low decompression rates. Earth Planet Sci Lett 501:192–201. https://doi.org/10.1016/j.epsl.2018.08.047

3. Ayers JC, Eggler DH (1995) Partitioning of elements between silicate melt and H2O–NaCl fluids at 1.5 and 2.0 GPa pressure: Implications for mantle metasomatism. Geochim Cosmochim Acta 59:4237–4246. https://doi.org/10.1016/0016-7037(95)00244-T

4. Bai TB, Koster van Groos AF (1999) The distribution of Na, K, Rb, Sr, Al, Ge, Cu, W, Mo, La, and ce between granitic melts and coexisting aqueous fluids. Geochim Cosmochim Acta 63:1117–1131. https://doi.org/10.1016/S0016-7037(98)00284-1

5. Bali E, Audétat A, Keppler H (2011) The mobility of U and Th in subduction zone fluids: an indicator of oxygen fugacity and fluid salinity. Contrib Mineral Petrol 161:597–613. https://doi.org/10.1007/s00410-010-0552-9