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