Forced folding of the neoautochthonous Late Cretaceous–Early Tertiary sequence at the western end of the Hatta Zone, Northern Oman Mountains-Reference-Cited by-同舟云学术

Forced folding of the neoautochthonous Late Cretaceous–Early Tertiary sequence at the western end of the Hatta Zone, Northern Oman Mountains

Published:2010-08-11 Issue:4 Volume:3 Page:369-393
ISSN:1866-7511
Container-title:Arabian Journal of Geosciences
language:en
Short-container-title:Arab J Geosci

Author:

Warrak Mohammed

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Link

http://link.springer.com/content/pdf/10.1007/s12517-010-0174-6.pdf

Reference58 articles.

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2. Ahmadhadi F, Lacombe O, Daniel JM (2007) Early reactivation of basement faults in Central Zagros (SW Iran): Evidence from pre-folding fracture populations in the Asmari Formation and Lower Tertiary paleogeography. In “ Thrust belts and foreland basins : from fold kinematics to hydrocarbon systems”. Lacombe O, Lavé J, Vergés J, Roure F (Eds), Frontiers in Earth Sciences, Springer-Verlag, New York chapter 11, 205–228.

3. Ahmadhadi F, Daniel J M, Azzizadeh M, Lacombe O (2008) Evidence for pre-folding vein development in the Oligo-Miocene Asmari Formation in the Central Zagros Fold Belt, Iran. Tectonics 27, TC1016, doi: 10.1029/2006TC001978

4. Bartlett WL, Friedman M, Logan JM (1981) Experimental folding and faulting of rocks under confining pressure, Part IX. Wrench faults in limestone layers. Tectonophysics 79:255–277

5. Boote DRD, Mou D, Waite RI (1990) Structural evolution of the Suneinah Foreland, Central Oman Mountains. In: Robertson AHF, Searle MP, Ries AC (eds) The Geology and Tectonics of the Oman Region, 49 Special Publication. Geological Society, London, pp 397–418

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