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)
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Title
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)
Authors
Keywords
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Journal
MINERALOGY AND PETROLOGY
Volume -, Issue -, Pages -
Publisher
Springer Science and Business Media LLC
Online
2020-09-05
DOI
10.1007/s00710-020-00721-z
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Note: Only part of the references are listed.- Two plutonic complexes of the Sanandaj-Sirjan magmatic-metamorphic belt record Jurassic to Early Cretaceous subduction of an old Neotethys beneath the Iran microplate
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