2015
DOI: 10.1016/j.oregeorev.2014.11.014
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Structural controls on the localization of Cu deposits in the Kerman Cu metallogenic province of Iran using geoinformatic techniques

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Cited by 12 publications
(6 citation statements)
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“…2014; Shafiei Bafti and Mohajjel, 2015). This tectonic event that prepared the suitable sites for emplacement of the granitic plutons and associated Cu deposits in a broad fault zone occurred during the emplacement of the Syn-to post Miocene granitic bodies into the volcanic and volcano-sedimentary sequences (Shafiei et al, 2009;Safari et al, 2015). Similar structural model that presented here for Sarduiyeh area, the fault duplexes as a major structure have been identified in the other Cu belts including the central Europe (Drew, 2005), Chuquicamata (Sibson, 1987), and Escondido deposits in northern Chile (Richards et al, 2001;Richards, 2003).…”
Section: Fault Kinematic Data and Structural Modelsupporting
confidence: 74%
See 1 more Smart Citation
“…2014; Shafiei Bafti and Mohajjel, 2015). This tectonic event that prepared the suitable sites for emplacement of the granitic plutons and associated Cu deposits in a broad fault zone occurred during the emplacement of the Syn-to post Miocene granitic bodies into the volcanic and volcano-sedimentary sequences (Shafiei et al, 2009;Safari et al, 2015). Similar structural model that presented here for Sarduiyeh area, the fault duplexes as a major structure have been identified in the other Cu belts including the central Europe (Drew, 2005), Chuquicamata (Sibson, 1987), and Escondido deposits in northern Chile (Richards et al, 2001;Richards, 2003).…”
Section: Fault Kinematic Data and Structural Modelsupporting
confidence: 74%
“…Evaluation of structural controls on Cu deposits has been investigated by structural geologists and covers a large part of applied structural geology to exploration and exploitation (Richards et al, 2001). Structural analysis in the main Cu belts revealed that the localization of the intrusions and associated Cu deposits are controlled by transpression (Cox, 1986;Cox et al, 1986;Tosdal and Richards, 2001;Safari et al, 2015). In this tectonic process, slip partitioning to the dipslip and strike-slip movements cause various structural domains such as fold-thrust belt and strike-slip domain on the overriding plate.…”
Section: Introductionmentioning
confidence: 99%
“…Some of the lithological units such as Oligocene granite and granodiorite, and Miocene-Pliocene andesite are the host rocks for porphyry copper mineralization which could determine possible copper mineralization within the study region. Faults are the main conduits of ascending fluids, and they provide porous zones in which metals can be trapped (Safari et al 2015;Mirzaie et al 2015). A maximum distance of 1000 m from a fault has been reported for copper mineralization within the study region (Derakhshani and Mchrabi 2009).…”
Section: Introductionmentioning
confidence: 90%
“…The Iju area, within 30 • 31 45 N to 30 • 33 05 N and 54 • 56 10 E to 54 • 57 30 E (Figure 1), is located 42 km NW of Shahre-Babak county, Kerman province, and 140 km NW of the Sarcheshme Cu mine. The Iju deposit is situated on the SE part of the Urmia-Dokhtar magmatic belt [41][42][43], which is characterized by numerous Cu deposits such as the Chah-Firouze, Sarcheshme, Meiduk, and Chah-Messi (Figure 1).…”
Section: Geologymentioning
confidence: 99%
“…Sarcheshme Cu mine. The Iju deposit is situated on the SE part of the Urmia-Dokhtar magmatic belt [41][42][43], which is characterized by numerous Cu deposits such as the Chah-Firouze, Sarcheshme, Meiduk, and Chah-Messi (Figure 1). The Iju deposit is situated in a mountainous area with Eocene-Paleocene pyroclastic volcanic rocks intruded by Miocene quartz-diorite and tonalite [44] (Figure 1).…”
Section: Geologymentioning
confidence: 99%