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)
Crossref DOI link: https://doi.org/10.1007/s00710-020-00721-z
Published Online: 2020-09-05
Published Print: 2020-12
Update policy: https://doi.org/10.1007/springer_crossmark_policy
Saki, Adel
Miri, Mirmohammad
Oberhänsli, Roland
Text and Data Mining valid from 2020-09-05
Version of Record valid from 2020-09-05
Article History
Received: 15 February 2020
Accepted: 12 August 2020
First Online: 5 September 2020