OJG  Vol.7 No.1 , January 2017
RETRACTED: Uprising Mechanism and Its Effects on the Evolution of Structural-Stratigraphic in the Mangerak Salt Dome (Firuzabad Fars-Iran)
ABSTRACT
Short Retraction Notice
The paper does not meet the standards of "Open Journal of Geology".
This article has been retracted to straighten the academic record. In making this decision the Editorial Board follows COPE's Retraction Guidelines. The aim is to promote the circulation of scientific research by offering an ideal research publication platform with due consideration of internationally accepted standards on publication ethics. The Editorial Board would like to extend its sincere apologies for any inconvenience this retraction may have caused.
Editor guiding this retraction: Prof. Alireza K. Somarin (Editorial Member of OJG)
The full retraction notice in PDF is preceding the original paper, which is marked "RETRACTED".

Cite this paper
  
References
[1]   Walpersdorf, A., Hatzeld, D., Nankali, H., Tavakoli, F., Nilforoushan, F., Tatar, M., Vernant, P., Chery, J. and Masson, F. (2007) Dofferece in GPS Deformation Pattern and Central Zagros (Iran).

[2]   Oveisi, B. (2010) Rares and Processes of Active Folding Evidenced by Pleistocene Terraces at the Central Zagros Front (Iran).

[3]   Bordenave, M.L. (2002) The Middle Cretaceous to Early Miocene Petroleum System in the Zagros Domain of Ira, and Its Prospect Evolution.

[4]   Koyi, H. (1988) Experimental Modeling of Role of Gravity and Lateral Shortening in Zagros Mountain Belt.

[5]   Lacombe, O., Mouthereau, F., Kargar, S. and Meyer, B. (2006) Late Cenozoic and Modern Stress Fields in the Western Fars (Iran): Implication for the Tectonic and Kinematic Evolution of Central Zagros.

[6]   Berberian, M. (1994) Master Blind Thrust Faults Hidden under the Zagros Folds: Active Basement Tectonics and Surface Morphotectonics.

[7]   Mouthereau, F., Lacombe, O. and Meyer, B. (2006) The Zagros Folded Belt (Fars, Iran): Constraints from Topography and Critical Wedge Modeling. Geophysical Journal International, 165, 336-356.
https://doi.org/10.1111/j.1365-246X.2006.02855.x

[8]   Snyder, D.B. and Barazangi, M. (1986) Deep Crustal Structure and Flexure of the Arabian Plate Beneath the Zagros Collisional Mountain Belt as Inferred from Gravity Observations. Tectonics, 5, 361-373.
https://doi.org/10.1029/TC005i003p00361

[9]   Talbot, C.J. (1998) Extrusions of Hormuz Salt in Iran.

[10]   Talbot, C.J., Medvedev, S., Alavi, M., Shahrivar, H. and Heidari, E. (2000) Salt Extrusion at Kuh-e-Jahani, Iran, from June 1994 to November 1997.

[11]   Tatar, M., Hatzfeld, D. and Ghafory-Ashtiany, M. (2003) Tectonics of the Central Zagros (Iran) Deduced from Microearthquake Seismicity. Geophysical Journal International, 156, 255-266.
https://doi.org/10.1111/j.1365-246X.2003.02145.x

[12]   Talebian, M. (2003) A Reappralisal of Earthquake Focal Mechanisms and Active Shortening in the Zagros Mountains of Iran. Geophysical Journal International, 156, 506-526.
https://doi.org/10.1111/j.1365-246X.2004.02092.x

[13]   Verges, J., Grelaud, S., Karpuz, R., Osthus, H., Nalpas, T., Shape, I., Guadarzi, H. (2002) Structure of the Zagros Mountain Front (Selurestan < Iran): Controls from Multiple Detachment Levels.

[14]   Evans, D.J. and Chadwick, R.A. (2009) Underground Gas Storage: Worldwide Experiences and Future Development in the UK and Europe. Special Publications No. 313, Geological Society, London.

[15]   Jackson, J.A. (1992) Partitioning of Strike-Slip and Convergentmotion between Eurasia and Arabia in Eastern Turkey and Caucasus. Journal of Geophysical Research, 97, 12471-12479.
https://doi.org/10.1029/92JB00944

[16]   Koyi, H.A. and Peterson, K. (1993) The Influence of Basement Faults on the Development of Salt Structures in the Danish Basin. Marine and Petroleum Geology, 10, 82-94.
https://doi.org/10.1016/0264-8172(93)90015-K

[17]   Ramsay, J.G. and Huber, M.I. (1987) The Techniques of Modern Structural Geology, Vol. 2: Folds and Fractures. Pergamon Press, London.

[18]   Suppe, J. (1984) Principles of Structural Geology. Department of Geological and Geophysical Sciences, Princeton University, Princeton.

 
 
Top