Doi.org/10.1016/j.epsl.2013.11.001
Revision as of 06:35, 18 August 2022 by 187.21.138.9 (talk) (Created page with "== Target Article == Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hydrogen isotope systematics of the Hakuba Happo hot spring; Suda, Konomi; et al.; Earth and Planetary Science Letters; 2014; https://doi.org/10.1016/j.epsl.2013.11.001 == Article providing comments == Hydrogen isotope fractionation in land-based serpentinization systems. Comment on “Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hyd...")
Target Article[edit | edit source]
Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hydrogen isotope systematics of the Hakuba Happo hot spring; Suda, Konomi; et al.; Earth and Planetary Science Letters; 2014; https://doi.org/10.1016/j.epsl.2013.11.001
Article providing comments[edit | edit source]
Hydrogen isotope fractionation in land-based serpentinization systems. Comment on “Origin of methane in serpentinite-hosted hydrothermal systems: The CH4–H2–H2O hydrogen isotope systematics of the Hakuba Happo hot spring” by Suda et al. [Earth Planet. Sci. Lett. 386 (2014) 112–125]; Whiticar, Michael J.; Etiope, Giuseppe; ; Earth and Planetary Science Letters; 2014-9-01 https://doi.org/10.1016/j.epsl.2014.06.004
Summary[edit | edit source]
Note: Opened to append information.