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Corrigendum to 'Multiple gas reservoirs are responsible for the gas emissions along the Marmara fault network'

Authors :
Claire Croguennec
Pete Burnard
Mathilde Pitel-Roudaut
David Madre
Jean-Pierre Donval
Bernard Marty
Louis Géli
Laurent Bignon
Ludovic Nicolas Legoix
Livio Ruffine
Pierre Henry
Yoan Germain
M. Namık Çağatay
Hailong Lu
Laboratoire Géosciences Océan (LGO)
Université de Bretagne Sud (UBS)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Centre de Recherches Pétrographiques et Géochimiques (CRPG)
Institut national des sciences de l'Univers (INSU - CNRS)-Université de Lorraine (UL)-Centre National de la Recherche Scientifique (CNRS)
College of Engineering [Beijing]
Peking University [Beijing]
Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)
Maden Fakültesi = Faculty of mines [Istanbul]
Istanbul Technical University (ITÜ)
Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE)
Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)
Source :
Deep Sea Research Part II: Topical Studies in Oceanography, Deep Sea Research Part II: Topical Studies in Oceanography, 2018, 153, pp.145-149. ⟨10.1016/j.dsr2.2018.12.002⟩, Deep Sea Research Part II: Topical Studies in Oceanography (0967-0645) (Elsevier BV), 2018-07, Vol. 153, P. 145-149
Publication Year :
2018
Publisher :
HAL CCSD, 2018.

Abstract

International audience; The authors regret a mistake on the value of δ13C of methane for one of the investigated gas samples. This concerns sample MRS-DV3-PE03, taken as end member and for which the correct methane δ13C value is -41.9‰ and not -34‰. The sample was collected at in situ pressure ( 100 bars) from a CO2-rich seep, in a liquid state. The mistake likely results from a partial extraction (i.e. done by expansion of the sampler volume to allow vaporization) of the pressurized sample for subsampling. Additional analyses have been carried out from fully vaporized samples. This error has resulted in updating the geochemical diagrams used for the discussion, and revising both the gas origin for sample MRS-DV3-PE03 and the section entitled "Delineation of sources, reservoirs or migration pathways, and estimation of level of mixing". The conclusion of the manuscript is unchanged. The authors would like to apologize for any inconvenience caused.

Details

Language :
English
ISSN :
09670645
Database :
OpenAIRE
Journal :
Deep Sea Research Part II: Topical Studies in Oceanography, Deep Sea Research Part II: Topical Studies in Oceanography, 2018, 153, pp.145-149. ⟨10.1016/j.dsr2.2018.12.002⟩, Deep Sea Research Part II: Topical Studies in Oceanography (0967-0645) (Elsevier BV), 2018-07, Vol. 153, P. 145-149
Accession number :
edsair.doi.dedup.....6fd8c458b42df8a278abe001fa48282a
Full Text :
https://doi.org/10.1016/j.dsr2.2018.12.002⟩