Structure of Masuleh Shear Zone: Evidence for Early–Middle Jurassic Dextral Shear Along Paleo-Tethys Suture Zone in the Western Alborz, NW Iran
Author:
Publisher
Pleiades Publishing Ltd
Subject
Geology
Link
http://link.springer.com/article/10.1134/S0016852118020073/fulltext.html
Reference57 articles.
1. A. Aghanabati, Geology of Iran (Geol. Surv. Iran, Tehran, 2004) [in Persian].
2. M. Alavi, “Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran,” Geol. Soc. Am. Bull. 103, 983–992 (1991).
3. M. Alavi, “Tectonostratigraphic synthesis and structural style of the Alborz Mountains system in northern Iran,” J. Geodyn. 21, 1–33 (1996).
4. M. Alavi, H. Vaziri, K. Seyed-Emami, and Y. Lasemi, “The Triassic and associated rocks of the Nakhlak and Aghdarband areas in central and northeastern Iran as remnants of the southern Turan active continental margin,” Geol. Soc. Am. Bull. 109, 1563–1575 (1997).
5. G. J. Axen, P. J. Lam, M. Grove, D. F. Stockli, and J. Hassanzadeh, “Exhumation of the west-central Alborz Mountains, Iran, Caspian subsidence and collision-related tectonics,” Geology 29, 559–562 (2001).
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1. Ediacaran to Jurassic geodynamic evolution of the Alborz Mountains, north Iran: geochronological data from the Gasht Metamorphic Complex;Swiss Journal of Geosciences;2024-08-28
2. Regional 3-D lithosphere structure of the northern half of Iran by local earthquake tomography;Geophysical Journal International;2020-09-11
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