Low-temperature catalytic CO2hydrogenation with geological quantities of ruthenium: a possible abiotic CH4source in chromitite-rich serpentinized rocks-Reference-Cited by-同舟云学术

Low-temperature catalytic CO2hydrogenation with geological quantities of ruthenium: a possible abiotic CH4source in chromitite-rich serpentinized rocks

Published:2014-09-18 Issue:3 Volume:15 Page:438-452
ISSN:1468-8115
Container-title:Geofluids
language:en
Short-container-title:Geofluids

Author:

Etiope G.¹²,Ionescu A.²^ORCID

Affiliation:

1. Istituto Nazionale di Geofisica e Vulcanologia; Sezione Roma 2 Italy

2. Faculty of Environmental Science and Engineering; Babes-Bolyai University; Cluj-Napoca Romania

Funder

Petrobras

Publisher

Wiley

Subject

General Earth and Planetary Sciences

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1111/gfl.12106/fullpdf

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4. Irreversible water-rock mass transfer accompanying the generation of the neutral Mg-HCO3 and high-pH, Ca-OH spring waters of the Génova province Italy;Bruni;Applied Geochemistry,2002

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