Cadomian Magmatic Rocks from Zarand (SE Iran) Formed in a Retro-Arc Basin
Abstract
A major arc-related magmatic episode is recorded in the Ediacaran-Early Cambrian (Cadomian) crust of Iran and Anatolia due to the southward subduction of Prototethyan oceanic lithosphere beneath N Gondwana. This magmatism was generated at a convergent margin, fragments of which can be traced for thousands of kilometres, from west Avalonia to the Lhasa terrane. Cadomian crustal tracts in Iran and Tauride-Anatolia are represented by abundant...
Paper Details
Title
Cadomian Magmatic Rocks from Zarand (SE Iran) Formed in a Retro-Arc Basin
Published Date
Aug 1, 2020
Journal
Volume
366-367
Pages
105569 - 105569
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