Accommodation of transpressional strain in the Arabia-Eurasia collision zone: new constraints from (U-Th)/He thermochronology in the Alborz mountains, north Iran

Author:

Ballato Paolo1,Stockli Daniel F.,Ghassemi Mohammad R.2,Landgraf Angela1,Strecker Manfred R.1,Hassanzadeh Jamshid3,Friedrich Anke4,Tabatabaei Saeid H.5

Affiliation:

1. Institut für Erd- und Umweltwissenschaften; Universität Potsdam; Potsdam; Germany

2. Research Institute for Earth Sciences; Geological Survey of Iran; Tehran; Iran

3. Division of Geological and Planetary Sciences; California Institute of Technology; Pasadena; California; USA

4. Institut für Geo- und Umweltwissenschaften; Ludwig-Maximilians Universität München; Munich; Germany

5. Building and Housing Research Center; Tehran; Iran

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference108 articles.

1. Faulting and Folding in Quaternary Deposits of Tehran's Piedmont (Iran);Abbassi;J. Asian Earth Sci,2009

2. Zagros orogeny: a subduction-dominated process;Agard;Geol Mag,2011

3. Aghanabati , A. A.R. Hamedi 1994 Geological map of Semnan quadrangle: Geological Survey of Iran, scale 1:250,000, 1 sheet

4. Inception of activity and slip rate on the Main Recent Fault of Zagros Mountains;Alipoor;Geomorphology,2012

5. Accommodation of late Cenozoic oblique shortening in the Alborz range, northern Iran;Allen;J. Struct. Geol.,2003

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