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Sar-Cheshmeh Deposit

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Journal Article
Published: 01 January 1994
Exploration and Mining Geology (1994) 3 (1): 39–43.
Journal Article
Journal: Economic Geology
Published: 01 May 1975
Economic Geology (1975) 70 (3): 568–576.
...G. C. Waterman; R. L. Hamilton Abstract The Sar Cheshmeh porphyry copper, located in southern Iran, was mined in ancient times, "rediscovered" about 1966, explored during 1966-1969, and will be in full production in 1977 at a rate of 40,000 tons of ore per day. Mineralization is associated...
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2016
DOI: 10.5382/SP.19.07
EISBN: 9781629499789
... advances in tectonic and paleogeographic reconstructions, and new geochronological and geochemical data reveal that in fact most of Iran’s major porphyry and epithermal deposits fall into this postsubduction category (e.g., Sungun, Sari Gunay, Meiduk, Sar Cheshmeh). The same applies to several major...
FIGURES | View All (8)
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2016
DOI: 10.5382/SP.19.08
EISBN: 9781629499789
...), Sar Cheshmeh (8.9 Mt Cu), and Reko Diq (23.0 Mt Cu) world-class porphyry deposits. Continued exploration for porphyry deposits in the region will likely lead to new discoveries in known porphyry belts, particularly under cover and below high- and intermediate-sulfidation epithermal systems...
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Journal Article
Published: 01 January 2002
Exploration and Mining Geology (2002) 11 (1-4): 43–48.
... ). The Darrehzar area is located southeast of the Sar Cheshmeh porphyry copper deposit. The topography around the deposit is mountainous. Detailed geophysical, geochemical and geological data was acquired by the Geological Survey of Iran (GSI, 1973) . The deposit was later studied by Maanijou (1993) , Ranjbar...
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Journal Article
Journal: Economic Geology
Published: 01 December 2006
Economic Geology (2006) 101 (8): 1455–1496.
... Eocene-Miocene Urumieh-Dokhtar calk-alkaline volcanic arc, which hosts several large porphyry Cu deposits (e.g., Sar Cheshmeh, Meiduk). Rocks of the Takab belt are also distinctly more alkaline than the Urumieh-Dokhtar rocks. Viewed in the context of plate tectonic models for Neogene closure of a Neo...
FIGURES | View All (23)
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2016
DOI: 10.5382/SP.19.13
EISBN: 9781629499789
... deposits (Sar Cheshmeh, Dexing, and Jiama), porphyry Cu-Mo deposits (Sungun and Qulong), and porphyry Mo deposits (Nannihu and Yuchiling; Fig. 1). These ore-forming intrusions crystallized from highly oxidized and hydrous melts with oxygen fugacity greater than FMQ +2 and water contents up to 12 wt...
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Journal Article
Journal: Geosphere
Published: 01 May 2006
Geosphere (2006) 2 (3): 161–186.
... mineral assessments. Semicircular patterns, 1–5 km in diameter, of mapped phyllic- and argillic-altered rocks are typically associated with Eocene to Miocene intrusive igneous rocks, some of which host known porphyry copper deposits, such as at Meiduk and Sar Cheshmeh. Linear phyllic-altered rock patterns...
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Image
Sketch map showing the position of the Central Iranian Volcanic Belt and po...
Published: 01 January 2002
Fig. 1. Sketch map showing the position of the Central Iranian Volcanic Belt and porphyry-type Cu deposits sub-parallel to the Zagros Thrust Zone ( Shahabpour, 1994 ). 1 – Bahreasman; 2 –Takht; 3 – Kuhe Panj; 4 – Darrehzar; 5 – Sar Cheshmeh; 6 – Mei-duk; 7 – Gowde kolvary; 8 – Darre Zereshg; 9
Journal Article
Published: 01 January 2005
Reviews in Mineralogy and Geochemistry (2005) 58 (1): 467–498.
... volcano-sedimentary complex and is bordered to the southwest by a major thrust zone and the Tertiary and Paleozoic sedimentary rocks of the Zagros Mountains ( Waterman and Hamilton 1975 ). The Sar Cheshmeh and Miduk copper deposits (mined by the National Iranian Copper Industries Company, NICICO) are two...
FIGURES | View All (7)
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2016
DOI: 10.5382/SP.19.09
EISBN: 9781629499789
... part of the Kerman belt ( Shafiei et al., 2009 ). Porphyry copper and skarn mineralization occurs throughout the Urumieh-Dokhtar magmatic belt and includes large deposits, such as Sar Cheshmeh, estimated at 1.2 Gt grading at 0.69% Cu, 0.03% Mo, 0.06 g/t Au, and 1.22 g/t Ag ( Shafiei and Shahabpour...
FIGURES | View All (15)
Image
Plot of Eu N /Eu N * vs. Mo (ppm) in zircons from Huojihe. Also shown for c...
Published: 01 March 2020
Figure 9. Plot of Eu N /Eu N * vs. Mo (ppm) in zircons from Huojihe. Also shown for comparison are compiled zircons from other porphyry deposits and barren igneous rocks. The porphyry Mo-bearing deposits include Sungun, Sar Cheshmeh, Jiama, Qulong, Yuchiling, Nannihu, and Dexing. The complied
Image
Geological map of <span class="search-highlight">Sar</span> <span class="search-highlight">Cheshmeh</span> area. 1 – Recent alluvium (Quaternary); 2 – ...
Published: 01 January 2002
Fig. 2. Geological map of Sar Cheshmeh area. 1 – Recent alluvium (Quaternary); 2 – Younger gravel fan (Quaternary); 3 – Calcareous terraces (Quaternary); 4 – Neogene sediments, mostly arenites with pebbles and boulders of volcanic and intrusive rocks, dacites and dacitic pyroclastics; 5
Image
Plots of ( a ) apatite δEu vs. δCe, ( b ) apatite Ga (ppm) vs. δEu, and ( c...
Published: 01 March 2020
, and Tongshanling. The compiled barren igneous rocks include the barren Weibao diorite porphyry, the barren Triassic Xiuwacu pluton, and the barren Zhongliao porphyritic granodiorite from Luoboling. For zircon, the complied porphyry Mo-bearing deposits include Sungun, Sar Cheshmeh, Jiama, Qulong, Yuchiling, Nannihu
Journal Article
Published: 01 January 2007
Exploration and Mining Geology (2007) 16 (1-2): 11–24.
... deposits in Iran (e.g., Sar-Cheshmeh, Sungun) are located in the central Iranian volcano-plutonic belt (CIVPB), also known as the Urumieh-Dokhtar belt. Darreh-Zerreshk (UTM 3495000E, 769000N) and Ali-Abad (UTM 3504800E, 769000N) are located ca. 60 km southwest of the city of Yazd, Yazd Province, in central...
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Image
Box plots of Ce 4+ /Ce 3+  versus Eu/Eu* for zircons from porphyry Cu depos...
Published: 01 August 2020
), Qulong Cu-Mo (QL), Jiama Cu-Mo (JA), Sar Cheshmeh Cu-Mo-Au (SC), and Sungun Cu-Mo (SG) deposits were calculated from Ce/Nd values reported by Lu et al. ( 2016 ) using the correlation Ce 4+ /Ce 3+ = 7.28 (Ce/Nd 1.35 ) determined in this study. Abbreviations are the same as those for Figures 9 and 10 .
Journal Article
Journal: Economic Geology
Published: 01 June 2013
Economic Geology (2013) 108 (4): 861–870.
... Cenozoic global cooling : Palaeogeography Palaeoclimatology Palaeoecology , v. 265 , p. 52 – 58 . Aminzadeh B. Shahabpour J. Maghami M. , 2011 , Variation of rhenium contents in molybdenites from the Sar Cheshmeh porphyry Cu-Mo deposit in Iran : Resource Geology , v. 61 , p. 290...
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Journal Article
Journal: Economic Geology
Published: 01 August 2005
Economic Geology (2005) 100 (5): 801–818.
... as copper ± molybdenum deposits in terms of contained metal. Four of the deposits are classified as copper-gold-molybdenum deposits (containing 0.1 g/t gold or more: La Escondida, Bingham, Sar Cheshmeh, and El Salvador), and four are copper-gold deposits (Grasberg, Cerro Colorado, Oyu Tolgoi, and Kal’makyr...
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Journal Article
Journal: Economic Geology
Published: 01 June 2010
Economic Geology (2010) 105 (4): 855–865.
... ; Kirkham and Dunne, 2000 ), although peak mineralization occurred during Miocene times ( Zarasvandi et al., 2005 ). The largest known porphyry copper deposits in Iran, Sungun (500 Mt at 0.75% copper) and Sar Cheshmeh (1,200 Mt at 1.2% copper; Ellis, 1991 ), are associated with Oligocene to Miocene...
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Image
Top: Map showing the locations of studied porphyry <span class="search-highlight">deposits</span>. The pie diagra...
Published: 01 December 2015
—Ridgeway; RB-LB—Rio Blanco–Los Bronces; SM—San Manuel; SR—Santa Rita; SC—Sar Cheshmeh; SE—Sierrita Esperanza; Su—Sungun; Td—Thames district; Ti—Tinggong; To—Toodoggone; Ty—Tyrone; Yu—Yulong. Bottom: Pressure ( P ) estimates obtained from FIs that homogenize by halite disappearance in porphyry deposits