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Paleomagnetism From Central Iran Reveals Arabia‐Eurasia Collision Onset at the Eocene/Oligocene Boundary.
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- Geophysical Research Letters, 2023, v. 50, n. 12, p. 1, doi. 10.1029/2023GL103858
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U–Pb age, Hf–O isotopes, and geochemistry of the Sardasht ophiolite in the NW Zagros orogen: Implications for the tectonic evolution of Neo‐Tethys.
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- Geological Journal, 2021, v. 56, n. 3, p. 1315, doi. 10.1002/gj.4011
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- Article
Petrology, geochemistry and tectonics of the extrusive sequence of Fannuj-Maskutan ophiolite, Southeastern Iran.
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- Journal of the Geological Society of India, 2015, v. 85, n. 5, p. 604, doi. 10.1007/s12594-015-0255-y
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Petrogenesis of Volcanic Rocks in the Khabr-Marvast Tectonized Ophiolite: Evidence for Subduction Processes in the South-Western Margin of Central Iranian Microcontinent.
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- Acta Geologica Sinica (English Edition), 2009, v. 83, n. 5, p. 884, doi. 10.1111/j.1755-6724.2009.00115.x
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