Quantitative kinematic analyses of the Darizhun shear zone within the hinterland of the Zagros orogenic belt, Iran

Author:

Derikvand Somaye

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference99 articles.

1. Agard P, Monie P, Gerber W et al (2006) Transient, synobduction exhumation of Zagros blueschists inferred from P-T, deformation, time and kinematic constraints: implications for Neotethyan wedge dynamics. J Geophy Res 111:B11401

2. Alavi M (1994) Tectonic of the Zagros orogenic belt of Iran: new data and interpretation. Tectonophysics 229:211–238

3. Alavi M (2007) Structures of the Zagros fold-thrust belt in Iran. Am J Sci 307:1064–1095

4. Alizadeh A, Sarkarinejad K, Sattarzadeh Y (2013) Kinematic vorticity analysis within the Zagros hinterland involved-basement window, Tutak gneiss dome, southwestern Iran. J Tethys 1:282–290

5. Allen M, Jackson J, Walker R (2004) Late Cenozoic reorganization of the Arabia-Eurasia collision and the comparison of short-term and long-term deformation rates. Tectonics 23:1–16

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