Constraints on fluid origins and migration velocities along the Marmara Main Fault (Sea of Marmara, Turkey) using helium isotopes

Type Article
Date 2012-08
Language English
Author(s) Burnard P.1, 7, Bourlange S.1, 2, Henry Pierre3, Geli LouisORCID4, Tryon M. D.5, Natal'In B.6, Sengor A. M. C.6, Ozeren M. S.6, Cagatay M. N.6
Affiliation(s) 1 : CRPG CNRS, F-54501 Vandoeuvre Les Nancy, France.
2 : Univ Lorraine, CRPG UPR2300, F-54501 Vandoeuvre Les Nancy, France.
3 : Aix Marseille Univ, CNRS, CEREGE, Coll France, F-13545 Aix En Provence 04, France.
4 : IFREMER, Marine Geosci Dept, F-29280 Plouzane, France.
5 : Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA.
6 : Istanbul Tech Univ, Fac Mines, Dept Geol, TR-34469 Istanbul, Turkey.
Source Earth And Planetary Science Letters (0012-821X) (Elsevier Science Bv), 2012-08 , Vol. 341-344 , P. 68-78
DOI 10.1016/j.epsl.2012.05.042
WOS© Times Cited 28
Keyword(s) fluids, gas emission, helium, Marmara Sea, North Anatolian Fault
Abstract Fluids venting from the submarine portion of the Marmara Main Fault (part of the North Anatolian Fault system, Turkey) were sampled in Ti bottles deployed by submersible. The fluids consist of mixtures of fault derived gases, fault related cold seep fluids, and ambient seawater; these components can readily be distinguished using the isotopes of He and the He/Ne ratios. He-3/He-4 ratios range between 0.03 +/- 0.1 and 4.9 +/- 0.4 Ra, indicating that both crustal and mantle derived sources of helium are sampled by the fault. The dominant gas in all the samples analyzed is methane with the abundance of CO2 below detection (<= 2%) in the mantle rich (high He-3/He-4) fluids. This is in contrast to nearly all mantle derived fluids where the C species are dominated by CO2. While high CH4/CO2 ratios may reflect organic or inorganic reactions within the crust which reduce mantle derived CO2 to methane, this is not a priori necessary: we show that simple dilution of mantle fluids with methane produced within local sediments could result in the high He-3/He-4, methane rich gases currently emanating from the fault. This observation is supported by an anticorrelation between He-3/He-4 and C/He-3, which is consistent with addition of C and He-4 simultaneously to the fluids. The highest He-3/He-4 ratios were found in the Tekirdag Basin, at the foot of the escarpment bordering the Western Sea of Marmara, where seismic data are consistent with the presence of a fault network at depth which could provide conduits permitting deep-seated fluids to rise to the surface. The lack of recent volcanism, or any evidence of underlying magmatism in the area, along with low temperature fluids, strongly suggests that the He-3-rich helium in these fluids was derived from the mantle itself with the Marmara Main Fault providing a high permeability conduit from the mantle to the surface. Assuming that the mantle source to the fluids originally had a He-3/He-4 ratio of 6 Ra, the minimum fluid velocities (considering only vertical transport and no mixing with parentless He-4) implied by the high He-3/He-4 ratios are of the order of 1-100 mm yr(-1). (C) 2012 Elsevier B.V. All rights reserved.
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Burnard P., Bourlange S., Henry Pierre, Geli Louis, Tryon M. D., Natal'In B., Sengor A. M. C., Ozeren M. S., Cagatay M. N. (2012). Constraints on fluid origins and migration velocities along the Marmara Main Fault (Sea of Marmara, Turkey) using helium isotopes. Earth And Planetary Science Letters, 341-344, 68-78. Publisher's official version : https://doi.org/10.1016/j.epsl.2012.05.042 , Open Access version : https://archimer.ifremer.fr/doc/00098/20954/