Oxidation of CH4 to CO2 and H2O by chloritization of detrital biotite at 270 ± 5 °C in the external part of the Central Alps, Switzerland

Lithos

Volumn 112, Issue 3-4, 2009, Pages 497-510

  Tarantola, A ^a,b   Mullis, J ^a   Guillaume, D ^c   Dubessy, J ^b   de Capitani, C ^a   Abdelmoula, M ^d  

^a UNIVERSITY OF BASEL   (Switzerland)

^b UNIVERSITÉ DE LORRAINE   (France)

^c CNRS   (France)

^d Laboratoire de Chimie Physique et Microbiologie pour l'Environnement   (France)

Author keywords

C O H fluids; CH4 H2O (CO2) transition zone; Chloritization; North Helvetic Flysch; Redox reactions

Indexed keywords

BIOTITE; CARBON DIOXIDE; CHLORITE; DETRITAL DEPOSIT; EXPERIMENTAL MINERALOGY; FLYSCH; METHANE; MOSSBAUER SPECTROSCOPY; MUSCOVITE; OXIDATION; P-T CONDITIONS; PHASE TRANSITION; REDOX CONDITIONS; REPLACEMENT; STABLE ISOTOPE; WATER;

ALPS; CENTRAL ALPS; CENTRAL EUROPE; EURASIA; EUROPE; SWITZERLAND;

EID: 70349134266     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2009.04.008     Document Type: Article

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