High temperature – low pressure metamorphism during subduction of Neo-Tethys beneath the Iranian plate: evidence for mafic migmatite formation in the Alvand complex (western Iran)-Reference-Cited by-同舟云学术

High temperature – low pressure metamorphism during subduction of Neo-Tethys beneath the Iranian plate: evidence for mafic migmatite formation in the Alvand complex (western Iran)

Published:2020-09-05 Issue:6 Volume:114 Page:539-557
ISSN:0930-0708
Container-title:Mineralogy and Petrology
language:en
Short-container-title:Miner Petrol

Author:

Saki Adel,Miri Mirmohammad,Oberhänsli Roland

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s00710-020-00721-z.pdf

Reference92 articles.

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3. Amidi M, Majidi B (1977) Geology map of Hamedan (1: 250,000). Geological survey of Iran, Tehran

4. Anders E, Grevesse N (1989) Abundances of the elements: meteoritic and solar. Geochim Cosmochim Acta 53:197–214

5. Azizi H, Asahara Y (2013) Juvenile granite in the Sanandaj–Sirjan zone, NW Iran: late Jurassic–early cretaceous arc–continent collision. Int Geol Rev 55:1523–1540

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