ArticlePhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2020
Chemical and isotopic analyses of hydrocarbon-bearing fluid inclusions in olivine-rich rocks.
Article in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.
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Who cites it
9 citing papers in PubMed, 71 citations in OpenAlex.
- Active conversion of atmospheric carbon dioxide to methane in peridotites of the Samail Ophiolite, Oman.Scientific reports · 2026Article
- Enigmatic HScientific reports · 2025Article
- Mineral carbonation of peridotite fueled by magmatic degassing and melt impregnation in an oceanic transform fault.Proceedings of the National Academy of Sciences of the United States of America · 2024Article
- The rocky road to organics needs drying.Nature communications · 2023Article
- Serpentinization as the source of energy, electrons, organics, catalysts, nutrients and pH gradients for the origin of LUCA and life.Frontiers in microbiology · 2023Review
- Massive abiotic methane production in eclogite during cold subduction.National science review · 2023Article
- Molecular Evidence for an Active Microbial Methane Cycle in Subsurface Serpentinite-Hosted Groundwaters in the Samail Ophiolite, Oman.Applied and environmental microbiology · 2021Article
- Six 'Must-Have' Minerals for Life's Emergence: Olivine, Pyrrhotite, Bridgmanite, Serpentine, Fougerite and Mackinawite.Life (Basel, Switzerland) · 2020Article
- Serpentinite in the Earth system.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2020Article
Corrections and comments
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Authors and funding
4 authors at 2 institutions in 1 country.
Funding
No grant is acknowledged in the PubMed record.
Abstract
We examined the mineralogical, chemical and isotopic compositions of secondary fluid inclusions in olivine-rich rocks from two active serpentinization systems: the Von Damm hydrothermal field (Mid-Cayman Rise) and the Zambales ophiolite (Philippines). Peridotite, troctolite and gabbroic rocks in these systems contain abundant CH
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