High-temperature water–rock interactions and hydrothermal environments in the chondrite-like core of Enceladus-Reference-Cited by-同舟云学术

High-temperature water–rock interactions and hydrothermal environments in the chondrite-like core of Enceladus

Published:2015-10-27 Issue:1 Volume:6 Page:
ISSN:2041-1723
Container-title:Nature Communications
language:en
Short-container-title:Nat Commun

Author:

Sekine Yasuhito,Shibuya Takazo,Postberg Frank,Hsu Hsiang-Wen,Suzuki Katsuhiko,Masaki Yuka,Kuwatani Tatsu,Mori Megumi,Hong Peng K.,Yoshizaki Motoko,Tachibana Shogo,Sirono Sin-iti

Publisher

Springer Science and Business Media LLC

Subject

General Physics and Astronomy,General Biochemistry, Genetics and Molecular Biology,General Chemistry

Link

http://www.nature.com/articles/ncomms9604.pdf

Reference70 articles.

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2. Postberg, F., Schmidt, J., Hillier, J., Kempf, S. & Srama, R. A salt-water reservoir as the source of a compositionally stratified plume on Enceladus. Nature 474, 620–622 (2011).

3. Waite, J. H. Jr et al. Liquid water on Enceladus from observations of ammonia and 40Ar in the plume. Nature 460, 487–490 (2009).

4. Schmidt, J., Brilliantov, N., Spahn, F. & Kempf, S. Slow dust in Enceladus’ plume from condensation and wall collisions in tiger stripe fractures. Nature 451, 685–688 (2008).

5. Hsu, H.-W. et al. Silica nanoparticles as an evidence of hydrothermal activities at Enceladus. Nature 519, 207–210 (2015).

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