The origin of rare alkali metals in geothermal fluids of southern Tibet, China: A silicon isotope perspective-Reference-Cited by-同舟云学术

The origin of rare alkali metals in geothermal fluids of southern Tibet, China: A silicon isotope perspective

Published:2019-05-27 Issue:1 Volume:9 Page:
ISSN:2045-2322
Container-title:Scientific Reports
language:en
Short-container-title:Sci Rep

Author:

Wang Wei,Wei Hai-Zhen^ORCID,Jiang Shao-Yong^ORCID,Tan Hong-Bing,Eastoe Christopher J.,Williams-Jones Anthony E.,Hohl Simon V.,Wu He-Pin

Funder

National Natural Science Foundation of China

the National Key R&D Program of China

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/s41598-019-44249-5.pdf

Reference49 articles.

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2. Zhang, Y. F. et al. A new geochemical perspective on hydrochemical evolution of the Tibetan geothermal system. Geochem. Int. 53, 1090–1106 (2015).

3. Palmer, M. R. & Sturchio, N. C. The boron isotope systematics of the Yellowstone National Park (Wyoming) hydrothermal system: A reconnaissance. Geochim. Cosmochim. Ac. 54, 2811–2815 (1990).

4. Hoke, L., Lamb, S., Hilton, D. R. & Poreda, R. J. Southern limit of mantle-derived geothermal helium emissions in Tibet: implications for lithospheric structure. Earth Planet Sc. Lett. 180, 297–308 (2000).

5. Symonds, R. B. & Reed, M. H. Calculation of multicomponent chemical-equilibria in gas-solid-liquid systems: Calculation methods, thermochemical data, and applications to studies of high temperature volcanic gases with examples from Mount St. Helens. Am. J. Sci. 293, 758–864 (1993).

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