Intra- to post-Messinian deep-water gas piping in the Levant Basin, SE Mediterranean

Ovie Emmanuel Eruteya, Nicolas Waldmann, Dagan Schalev, Yizhaq Makovsky, Zvi Ben-Avraham

Research output: Contribution to journalArticlepeer-review


This study presents evidences for fluid flow manifested as pipe structures in the post-evaporitic overburden characterised from a 3D seismic data from the Levant Basin, offshore central Israel. Interestingly these pipes are genetically and spatially contextualized east and west of the study area, all rooted in the Messinian evaporite substratum. Pipes in the western group accounts for 83% of the pipe population, are crudely cylindrical, oval to elliptical in planform, with diameter and height ranging ~350-2000 m and ~320-420 m, respectively. Internal configurations within this group varies from chaotic to concave upward reflections diagnostic of fluid induced collapse. Pipes in the eastern group are seepage pipes appearing conical in shape, with height of ~350-510 m and diameter of ~320-420 m. The eastern group pipes are characterized by lack of internal reflectivity and/or disrupted stratal reflections. The western group indicates an episode of fluid flow till the mid-Pliocene, compared to late Pliocene in the eastern group. A conceptual model for the pipes in the western group is proposed to have occurred from subjacent dissolution of the Messinian evaporite under deep-water marine conditions during the Pliocene by vertically focused fluid flow from intra-Messinian realm dissolving the top evaporites and inducing systematic collapse in the overburden, the onset of which may have been triggered by seismicity. Conversely, pipes in the eastern group are proposed to have developed from breaching the top evaporite by pressurized fluids that developed from lateral pressure transfer due to differential loading of the overburden and salt tectonics. These pipe structures may pose a potential risk to deep-water exploration and development. The fluid expulsion phenomena documented in this study has wider implications for the hydrodynamics of many basins where thick evaporite layers are widely developed.

Original languageEnglish
Pages (from-to)246-261
Number of pages16
JournalMarine and Petroleum Geology
StatePublished - 1 Sep 2015

Bibliographical note

Funding Information:
The authors are grateful to ILDC, Modi'in Energy and GGR for graciously granting permission to show the geophysical dataset. We would like to thank Joe Cartwright and Annalisa Iadanza for their skilled, extremely careful and constructive review which improved the outlook of this paper. Special thanks also to guest editors Jean-Pierre Suc and Namık Çağatay for their useful comments. Ovie is grateful to the Graduate Studies Authority, University of Haifa and Marie Curie Career Integration Grants (CIG) FP7-PEOPLE-2011-CIG in the framework of Nicolas Waldmann's GASTIME project, for funding towards his doctoral studies. We are very grateful to Uri Schattner and Moshe Reshef for fruitful discussions at the inception of this study. We also thank Schlumberger, Paradigm and IHS Kingdom for granting academic licenses of their respective seismic processing and interpretation software packages to the Department of Marine Geosciences, University of Haifa. Gil Tsioni, Omri Gadol, Lee Stern, Reli Wald and Lisa Coianiz are thanked for helping with the geospatial data presented. Nimer Taha is thanked for technical support at the PetroLab. Ovie likes to thank Oghene for his guidance and also Dr. Jonathan Eruteya and Eunice Eruteya for their support during the preparation of this contribution.

Publisher Copyright:
© 2015 Elsevier Ltd.


  • Deep-water geohazards
  • Deep-water salt tectonics
  • Evaporite dissolution
  • Fluid flow
  • Levant Basin
  • Messinian salinity crisis
  • Pipes

ASJC Scopus subject areas

  • Oceanography
  • Geophysics
  • Geology
  • Economic Geology
  • Stratigraphy


Dive into the research topics of 'Intra- to post-Messinian deep-water gas piping in the Levant Basin, SE Mediterranean'. Together they form a unique fingerprint.

Cite this