Corrigendum to “Multiple gas reservoirs are responsible for the gas emissions along the Marmara fault network”
| Type | Article | ||||||||||||
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| Date | 2018-07 | ||||||||||||
| Language | English | ||||||||||||
| Author(s) | Ruffine Livio 1, Donval Jean-Pierre1, Croguennec Claire1, Burnard Pete2, 8, Lu Hailong3, Germain Yoan1, Legoix Ludovic N.1, 4, Bignon Laurent5, Çağatay M. Namık6, Marty Bernard2, Madre David2, Pitel-Roudaut Mathilde1, Henry Pierre7, Géli Louis1 |
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| Affiliation(s) | 1 : IFREMER, Département Ressources physiques et Ecosystèmes de fond de Mer (REM), Unité des Géosciences Marines, 29280 Plouzané, France 2 : Centre de Recherches Pétrographiques et Géochimiques, Unité Mixte de Recherches CNRS & Université de Lorraine, F-54500 Vandoeuvre-lès-Nancy, France 3 : Peking University, Department of Energy & Sciences, College of Engineering, Beijing 100871 4 : GEOMAR Helmholtz Centre for Ocean Research Kiel, Wischhofstr. 1-3, D-24148 Kiel, Germany 5 : IFREMER, Département Ressources physiques et Ecosystèmes de fond de Mer (REM), Unité des Recherches et Développements Technologiques, 29280 Plouzané, France 6 : Istanbul Teknik University, Faculty of Mines, EMCOL and Department of Geological Engineering, TR-34469 Istanbul, Turkey 7 : Aix-Marseille Univ., CNRS, IRD, Coll. France, CEREGE, Aix-en-Provence, France 8 : Centre de Recherches Pétrographiques et Géochimiques, Unité Mixte de Recherches CNRS & Université de Lorraine, F-54500 Vandoeuvre-lès-Nancy, France |
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| Source | Deep Sea Research Part II: Topical Studies in Oceanography (0967-0645) (Elsevier BV), 2018-07 , Vol. 153 , P. 145-149 | ||||||||||||
| DOI | 10.1016/j.dsr2.2018.12.002 | ||||||||||||
| Abstract | 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. |
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