Evidence for pre-folding vein development in the Oligo-Miocene Asmari Formation in the Central Zagros Fold Belt, Iran-Reference-Cited by-同舟云学术

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Evidence for pre-folding vein development in the Oligo-Miocene Asmari Formation in the Central Zagros Fold Belt, Iran

Published:2008-02 Issue:1 Volume:27 Page:n/a-n/a
ISSN:0278-7407
Container-title:Tectonics
language:en
Short-container-title:Tectonics

Author:

Ahmadhadi Faram¹,Daniel Jean-Marc²,Azzizadeh Mehran³,Lacombe Olivier⁴

Affiliation:

1. Iranian Offshore Oil Company (IOOC), Geology & Petrophysics Department; Tehran; Iran

2. Institut Français de Pétrole (IFP); Rueil-Malmaison Cedex; France

3. RIPI; West Blvd., Azadi Sports Complex; Tehran; Iran

4. Université P. & M. Curie - Paris 6, Laboratoire de Tectonique; UMR 7072 CNRS; Paris Cedex; France

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference80 articles.

1. Interaction of the Zagros fold-thrust belt and the Arabian-type, deep-seated folds in the Abadan Plain and the Dezful Embayment, SW Iran;Abdollahie;Petrol. Geosci.,2006

2. Convergence history across Zagros, Iran; constraints from collisional and earlier deformation;Agard;Geologische Rundschau = Int. J. Earth Sci. 1999. Print,2005

3. Early Reactivation of Basement Faults in Central Zagros (SW Iran): Evidence from Pre-folding Fracture Populations in Asmari Formation and Lower Tertiary Paleogeography

4. Tectonics of the Zagros orogenic belt of Iran: New data and interpretations;Alavi;Tectonophysics,1994

5. Analysis of microstructures in the Meade Plate of the Idaho-Wyoming foreland thrust belt, U.S.A.;Allmendinger;Tectonophysics,1982

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