2010
DOI: 10.1127/0077-7749/2009/0017
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Metamorphism and metasomatism in the Jurassic Nain ophiolitic melange, Central Iran

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Cited by 16 publications
(7 citation statements)
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“…These ophiolites are highly dismembered and sliced, and characterized as tectonic mélanges. The spreading of this ocean commenced in the Triassic and terminated in the Eocene (Torabi 2003; Shirdashtzadeh et al. 2009).…”
Section: Discussionmentioning
confidence: 99%
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“…These ophiolites are highly dismembered and sliced, and characterized as tectonic mélanges. The spreading of this ocean commenced in the Triassic and terminated in the Eocene (Torabi 2003; Shirdashtzadeh et al. 2009).…”
Section: Discussionmentioning
confidence: 99%
“…These ophiolites are highly dismembered and sliced, and characterized as tectonic mélanges. The spreading of this ocean commenced in the Triassic and terminated in the Eocene (Torabi 2003;Shirdashtzadeh et al 2009). Therefore, the former subduction of the CEIM confining oceanic crust and dehydration or melting of the subducted slab is the best candidate for the mechanism of upper mantle metasomatism.…”
Section: Tectonic Settingmentioning
confidence: 99%
“…Agard et al, 2011, and references therein). Glennie (1992), Torabi (2004), Reichert (2007), Shirdashtzadeh et al (2010Shirdashtzadeh et al ( , 2011Shirdashtzadeh et al ( , 2014 considered the eastern branch of the Neo-Tethyan Ocean (or Nain-Baft Ocean in Ghasemi andTalbot, 2006, andShirdashtzadeh et al, 2011), opened from southeast Turkey to Oman and separated the Sanandaj-Sirjan and Central Iranian plates (Fig. 1A), from the approximately Early Jurassic to the late Early CretaceousPaleocene.…”
Section: Introductionmentioning
confidence: 96%
“…Two oceanic crust subduction events are the cause of incompatible element enrichment of the mantle and the Oligocene alkaline magmatism in the northwest of CEIM: (i) northeastward Neotethys subduction along the Zagros Thrust Zone (ZTZ) beneath central Iran from the Triassic to the Eocene (Torabi 2010); and (ii) subduction of an oceanic crust along the Great Kavir Fault, which lies to the west of the CEIM. The spreading of the last ocean commenced in the Triassic and terminated in the Eocene (Shirdashtzadeh et al 2009). The remnants of this oceanic crust are as ophiolitic mélanges (e.g.…”
Section: Tectonic Settingmentioning
confidence: 96%