Dataset for H 2 , CH 4 and organic compounds formation during experimental serpentinization
Author:
Affiliation:
1. Tetherless World Constellation Rensselaer Polytechnic Institute Troy NY USA
2. CSIRO Mineral Resources Kensington WA Australia
3. Univ LyonUniv Lyon 1ENSLCNRSLGL‐TPE Villeurbanne France
4. Total CSTJF Pau France
Funder
Total
Alfred P. Sloan Foundation
Publisher
Wiley
Subject
General Earth and Planetary Sciences
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1002/gdj3.105
Reference62 articles.
1. Compositional controls on vent fluids from ultramafic-hosted hydrothermal systems at mid-ocean ridges: An experimental study at 400°C, 500 bars
2. Aluminum speeds up the hydrothermal alteration of olivine
3. A Review of H2, CH4, and Hydrocarbon Formation in Experimental Serpentinization Using Network Analysis
4. Geochemical Evidence of Present-Day Serpentinization
5. Reduction of CO2 during serpentinization of olivine at 300 °C and 500 bar
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1. Forms and fluxes of carbon: Surface to deep;Reference Module in Earth Systems and Environmental Sciences;2024
2. Microbial vs abiotic origin of methane in continental serpentinized ultramafic rocks: A critical review and the need of a holistic approach;Applied Geochemistry;2022-08
3. Molecular hydrogen in surface and subsurface natural gases: Abundance, origins and ideas for deliberate exploration;Earth-Science Reviews;2022-07
4. Database on mineral mediated carbon reduction: implications for future research;International Journal of Astrobiology;2022-06-30
5. Cobalt: A must-have element for life and livelihood;Proceedings of the National Academy of Sciences;2022-01-13
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