Strain Geometry and Vorticity Analysis of the Deformed Radiolarian Rocks in the Abade-Tashk Area, the Zagros Suture Zone, Iran
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
https://link.springer.com/content/pdf/10.1007/s12583-021-1606-9.pdf
Reference104 articles.
1. Agard, P., Monié, 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. Journal of Geophysical Research: Solid Earth, 111(B11): B11401. https://doi.org/10.1029/2005jb004103
2. Agard, P., Omrani, J., Jolivet, L., et al., 2011. Zagros Orogeny: A Subduction-Dominated Process. Geological Magazine, 148(5/6): 692–725. https://doi.org/10.1017/s001675681100046x
3. Ajirlu, M. S., Moazzen, M., Hajialioghli, R., 2016. Tectonic Evolution of the Zagros Orogen in the Realm of the Neotethys between the Central Iran and Arabian Plates: An Ophiolite Perspective. Central European Geology, 59(1/2/3/4): 1–27. https://doi.org/10.1556/24.59.2016.001
4. Alavi, M., 1994. Tectonics of the Zagros Orogenic Belt of Iran: New Data and Interpretations. Tectonophysics, 229(3/4): 211–238. https://doi.org/10.1016/0040-1951(94)90030-2
5. Babaei, A., Babaie, H. A., Arvin, M., 2005. Tectonic Evolution of the Neyriz Ophiolite, Iran: An Accretionary Prism Model. Ofioliti, 30(2): 65–74
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