U-Pb zircon ages and geochemistry of Kangareh and Taghiabad mafic bodies in northern Sanandaj-Sirjan Zone, Iran: Evidence for intra-oceanic arc and back-arc tectonic regime in Late Jurassic
The Kangareh and Taghiabad bodies are mainly mafic rocks in the northwest Iran.
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87Sr/86Sr and 143Nd/144Nd ratios infer depleted mantle source for these bodies.
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Chemical and isotope ratios confirm the intra-oceanic regime for these rocks.
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Our finding infers the accretion-type of continental growth of western of Iran.
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