2010
DOI: 10.1016/j.oregeorev.2010.05.004
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Lead isotope signatures of the igneous rocks and porphyry copper deposits from the Kerman Cenozoic magmatic arc (SE Iran), and their magmatic-metallogenetic implications

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Cited by 73 publications
(28 citation statements)
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“…Geochemical data for the weakly mineralized late Eoceneearly Oligocene Jebal Barez and strongly mineralized middle to late Miocene Kuh Panj plutonic suites indicate emplacement in thicker crust and greater assimilation of crustal materials by the later suite (Shafiei and others, 2009;Shafiei, 2010).…”
Section: Magmatismmentioning
confidence: 99%
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“…Geochemical data for the weakly mineralized late Eoceneearly Oligocene Jebal Barez and strongly mineralized middle to late Miocene Kuh Panj plutonic suites indicate emplacement in thicker crust and greater assimilation of crustal materials by the later suite (Shafiei and others, 2009;Shafiei, 2010).…”
Section: Magmatismmentioning
confidence: 99%
“…Middle to late Eocene unconformable deposition of back-arc volcaniclastic sequences with interbedded bi-modal volcanic rocks of the Razak complex, followed by high-K calc-alkaline Jebal Barez gabbroic to granitic intrusions with primitive arc signatures (Shafiei, 2010). The Jebal Barez plutons occur throughout the Kerman arc segment, but they are most widespread in its southern parts (Shafiei and others, 2008).…”
Section: Magmatismmentioning
confidence: 99%
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