1987
DOI: 10.1007/bf00204520
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Lead isotope data from the Sar-Cheshmeh porphyry copper deposit, Iran

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Cited by 85 publications
(48 citation statements)
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“…This deposit is located in SE part of main Iranian Cenozoic magmatic belt, named Urumieh-Dokhtar, and extends 1700 km and 150 km wide from NW to SE Iran, as shown in Fig. 1 (Alavi, 1994;Shahabpour, 1994;Alavi, 2004;Dargahi et al, 2010;. This belt has been interpreted to be a subduction related Andean-type magmatic arc that has been active from the Late Jurassic to the present.…”
Section: Geological Setting Of Case Studymentioning
confidence: 99%
“…This deposit is located in SE part of main Iranian Cenozoic magmatic belt, named Urumieh-Dokhtar, and extends 1700 km and 150 km wide from NW to SE Iran, as shown in Fig. 1 (Alavi, 1994;Shahabpour, 1994;Alavi, 2004;Dargahi et al, 2010;. This belt has been interpreted to be a subduction related Andean-type magmatic arc that has been active from the Late Jurassic to the present.…”
Section: Geological Setting Of Case Studymentioning
confidence: 99%
“…These two porphyry copper prospects (Bazin and Hübner, 1969a;Förster, 1978;Shahabpour and Kramers, 1987) are mentioned in the literature. However, little is known about their geology, alteration, mineralization, and resource base.…”
Section: South Of Ardestan and Sharif Abad Porphyry Prospectsmentioning
confidence: 99%
“…The quartz-sericite zone extends down to 400 m and outward into the host rocks, where it is the strongest and corresponds roughly with the 0.4 percent copper grade boundary. Propylitization surrounds the entire complex and grades outward into unaltered andesite (Shahabpour and Kramers, 1987).…”
Section: Sar Cheshmeh Porphyry Depositmentioning
confidence: 99%
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“…The northwestern part of the Urumieh-Dkhtar magmatic arc is the product of Tethys oceanic plate subducted under the Iranian microplate followed by continentto-continent collision of the Arabian and Eurasian plates (Regard et al, 2004). Urumieh-Dokhtar belt is the host of large porphyry copper deposits such as Sungun in NW part, Kahang and Darre Zereshk in middle part and Meiduk and Sarcheshmeh in SE part (Shahabpour, 1994). These deposits were formed by intrusion of granodiorite-diorite stocks into Upper Cretaceous-Eocene andesitic volcano-sedimentary rocks.…”
Section: Geological and Petrological Studies Of Khatun Abad Areamentioning
confidence: 99%