Repeated magmatic buildup and deep “hot zones” in continental evolution: The Cadomian crust of Iran
Earth and Planetary Science Letters(2020)
Abstract
•Cadomian continental arc crust of NE Iran was built during ∼15 Myr of magmatism.•Magmatic flare-up in Iran Cadomia occurred over ∼45 Myr; 570 to 525 Ma.•Geochemical differentiation in “hot zones” built the stratified continental crust of Iran.
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Key words
continental crust,magmatic flare-up,hot zone,Cadomian,Iran
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