The influence of silica on reaction rates and molecular hydrogen (H2) generation during olivine hydrothermal alteration-Reference-Cited by-同舟云学术

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The influence of silica on reaction rates and molecular hydrogen (H2) generation during olivine hydrothermal alteration

Published:2023-12-15 Issue:1 Volume:67 Page:222-233
ISSN:1674-7313
Container-title:Science China Earth Sciences
language:en
Short-container-title:Sci. China Earth Sci.

Author:

Huang Ruifang,Sun Weidong,Ding Xing,Zhao Yusheng,Li Yibing,Shang Xiuqi

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

https://link.springer.com/content/pdf/10.1007/s11430-023-1172-9.pdf

Reference63 articles.

1. Allen D E, SeyfriedJr W E. 2003. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 bars. Geochim Cosmochim Acta, 67: 1531–1542

2. Andreani M, Muñoz M, Marcaillou C, Delacour A. 2013. μXANES study of iron redox state in serpentine during oceanic serpentinization. Lithos, 178: 70–83

3. Bach W, Garrido C J, Paulick H, Harvey J, Rosner M. 2004. Seawater-peridotite interactions: First insights from ODP Leg 209, MAR 15°N. Geochem Geophys Geosyst, 5: Q09F26

4. Beard J S, Frost B R, Fryer P, McCaig A, Searle R, Ildefonse B, Zinin P, Sharma S K. 2009. Onset and progression of serpentinization and magnetite formation in olivine-rich troctolite from IODP Hole U1309D. J Petrol, 50: 387–403

5. Berndt M E, Allen D E, Seyfried W EJr. 1996. Reduction of CO2 during serpentinization of olivine at 300°C and 500 bar. Geology, 24: 351–354

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