Cu-Ag Besshi type volcanogenic massive sulfide mineralization in the Late Cretaceous volcano- sedimentary sequence: the case of Garmabe Paein deposit, southeast of Shahrood

زمین شناسی اقتصادی

Article 7, Volume 9, Issue 1 - Serial Number 16, July 2017, Pages 213-233   

Document Type: Research Article

DOI: 10.22067/econg.v9i1.43062

Authors

Majid Tashi^* ; Fardin Mousivand; Habibollah Ghasemi

Shahrood University of Technology

Abstract

Introduction
Iran hosts numerous types of Volcanogenic massive sulfide (VMS) deposits that occur within different tectonic assemblages and have formed at discrete time periods (Mousivand et al. 2008). The Sabzevar zone hosts several VMS deposits including the Nudeh Cu-Ag deposit (Maghfouri, 2012) and some deposits in the Kharturan area (Tashi et al., 2014), and the Kharturan area locates in the Sabzevar subzone of the Central East Iranian Microcontinent. The Sabzevar subzone mainly involves Mesozoic and Cenozoic rock unites. The Late Cretaceous ophiolite mellanges and volcano-sedimentary sequences have high extension in the Subzone. Based on Rossetti (Rossetti et al. 2010), the Cretaceous rock units were formed in a back-arc setting due to subduction of the Neo-Tethyan oceanic crust beneath the Iranian plate. The exposed rock units of the Kharturan area from bottom to top are dominated by Early Cretaceous, orbitolina-bearing massive limestone, dacitic-andesitic volcanics and related volcaniclastic rocks٫ chert and radiolarite and Late Cretaceous globotrunkana- bearing limestone, paleocene polygenic conglomerate consisting of the Cretaceous volcanics and limestone pebbles (equal to the Kerman conglomerate), and Pliocene weakly-cemented polygenic conglomerate horizon. The Garmabe Paein copper-silver deposit and the Asbkeshan deposit and a few occurrences, are located at 290 km southeast of Shahrood and they have occurred within the Upper Cretaceous volcano-sedimentary sequence in the Sabzevar subzone. The aim of this study is to discuss the genesis of the Garmabe Paein deposit based on geological, textural and structural, mineralogical and geochemical evidence.

Materials and methods
A field study and sampling was performed during the year 2013. During the field observations, 94 rock samples were collected from the study area, and 45 thin sections were prepared and studied using a polarizing microscope. Also, 5 samples for the XRD method, 21 samples for the XRF and ICP-OES methods were analyzed in the Iranian Mines and Mining Industries Development and Renovation (IMIDRO) Company labs.

Results
The Garmabe Paein copper-silver deposit is located in the Sabzevar subzone of the Late Cretaceous Volcanio-sedimentary sequence. This mineralization occurred as stratiform and stratabound in a specific stratigraphic horizon. The host rocks of mineralization are andesitic-dacitic volcanic rocks and their related volcaniclastics. The mineralization occurred as four ore facies, from footwall to hanging wall: vein-veinlet-s (stringer), massive, bedded and exhalites. Ore textures and structures involve massive, semi-massive, laminated, banded, vein-veinlets, replacement and open space fillings. Minerlogically, the deposit contains primary minerals such as pyrite, chalcopyrite and magnetite, and secondary minerals such as native copper, cuprite, covellite, malachite and Fe-Mn oxides. Wallrock alterations are dominated by chloritic and minor siliceous and argillic. The highest grades of gold and silver in the deposit are 1 and 19 grams per ton, respectively. The amounts of Zn, Pb, Au, As, Ag and Mn increase from the stringer to the upper part of the deposit. It seems that the occurrence of submarine volcanic activity in the Late Cretaceous back- arc basin have resulted in the deposition of this Besshi type massive sulfide deposit.

Discussion
Most of characteristics of the Garmabe Paein Cu-Ag deposit including tectonic setting, geological environment, host rocks, geometry, textural and structural, mineralogical and geochemical features, are very similar to those of the Besshi- or pelitic mafic-type (Franklin et al., 2005) volcanogenic massive sulfide (VMS) deposits.

Acknowledgements
The authors are grateful to the University of Shahrood Grant Commission for research funding and the IMIDRO Company.

References
Franklin, J.M., Gibson, H.L., Galley, A.G. and Jonasson, I.R., 2005. Volcanogenic massive sulfide deposits. In: J.W. Hedenquist, J.F.H. Thompson, R.J. Goldfarb and J.P. Richads (Editors), Economic Geology 100th Anniversary Volume. Society of Economic Geologists, Littleton, Colorado, pp.523-560.
Maghfouri, S., 2012. Geology, mineralogy, geochemistry and genesis of Cu mineralization Within Late Cretaceous Volcano- sedimentary sequence in southwest of Sabzevar, with emphasis on the Nudeh deposit. M.Sc. Thesis, Tarbit Modares University, Tehran, Iran, 312 pp. (In Persian with English abstract)
Mousivand, F., Rastad, E. and Peter, J.M., 2008. An overview of volcanogenic massive sulfide deposits of Iran. 33rd International Geology Congress Oslo, Oslo, Norway.
Rossetti, F., Nasrabady, M., Vignaroli, G., Theye, T., Gerdes, A., Razavi, M. and MoinVaziri, H., 2010. Early Cretaceous migmatitic mafic granulites from the Sabzevar range (NE Iran): implications for the closure of the Mesozoic peri- Tethyan oceans in central Iran. Journal of Terra Nova, 22(1): 26-34.
Tashi, M., Mousivand, F. and Ghasemi, H., 2014. Volcanogenic massive sulfide Cu-Ag mineralization in the Kharturan area, southeast of Shahrood. 1th International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Silk Road Higher Education Cooperation Forum, China University of Geosciences (Wuhan), Wuhan, China.

Keywords

Volcanogenic massive sulfide; Besshi type; Garmabe Paein; Late Cretaceous; Sabzevar subzone

References

Aghanabati, S.A., 2004. Geological of Iran. Geological Survey of Iran,Tehran, 709 pp.

Alavi, M., 1994. Sedimentary and structural characteristics of the Paleo-Tethys remnants in northeastern Iran. Geological Society of America Bulletin, 103(8): 983- 992.

Badrzadeh, Z., Sabzehei, M., Rastad, E., Emami, M.H. and Gimeno, D., 2010. Various stages of sulfidemineralization in Sargaz Volcanogenic massive sulfide deposit, Northwest Jirft, Southern Sanandaj-Sirjan. Scientific Quarter Journal Geosciences. Geology Surrveyof Iran, 76(19): 85-94. (in Persian with English abstract)

Dergatchev, A., Eremin, N.I. and Sergeeva, N.E., 2010. Volcanogenic massive sulfide deposit of ophiolite associations. Journal of Moscow University Geology Bulletin, 65(5): 265–272.

Franklin, J.M., Gibson, H.L., Galley, A.G. and Jonasson, I.R., 2005. Volcanogenic massive sulfide deposits. In: J.W. Hedenquist, J.F.H. Thompson, R.J. Goldfarb and J.P. Richads (Editors), Economic Geology 100th Anniversary Volume. Society of Economic Geologists, Littleton, Colorado, pp.523-560.

Galley, A.G., 2003. Composite synvolcanic intrusions associated with Precambrian VMS- related hydrothermal systems. Journal of Mineral Deposita, 38(4): 443-473.

Galley, A.G., Hannington, M.D. and Jonasson, I.R., 2007. Volcanogenic massive sulfide deposit. In: W.D. Goodfellow (Editor), Mineral Deposit of Canada: A Synthesis of Major Deposit Types, District Metalogeny, the Evolution of Geological Province, and Exploration Methods. Mineral Deposits Division, Geological Association of Canada, Ontario, pp. 141- 161.

Ghaemi, F. and Moussavi Harami, R., 2007. Geology map of Doruneh, scale 1:100,000. Geological Survey of Iran

Gibson, H. and Galley, A., 2007. Volcanogenic massive sulphide deposits of the Archean, Noranda District, Quebec. In: W.D. Goodfellow (Editor), Mineral Deposits of Canada: A Synthesis of Major Deposit-types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods. Mineral Deposits Division, Geological Association of Canada, Ontario, pp. 533-552.

Goodfellow, W.D., 2007. Metallogeny of the Bathurst Mining Camp, northern New Brunswick. In: W.D. Goodfellow (Editor), Mineral Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods. Mineral Deposits Division. Geological Association of Canada, Ontario, pp. 449-469.

Kohansal, R., 2008. Geological map of Marry-Asbkeshan, scale 1:100,000. Geological Survey of Iran.

Maghfouri, S., 2012. Geology, mineralogy, geochemistry and genesis of Cu mineralization Within Late Cretaceous Volcano- sedimentary sequence in southwest of Sabzevar, with emphasis on the Nudeh deposit. M.Sc. Thesis, Tarbit Modares University, Tehran, Iran, 312 pp. (In Persian with English abstract)

Malekzadeh shfarodi, A., Karimpour, M.H. and Mazaheri. S., 2005. Geology, mineralogy and geochemistry of Taknar polimetal (Cu-Zn-Au-Ag-Pb) deposit (Tak-I) in the Khorasan-Bardaskan. Journal of Iran society crystallography and mineralogy, 12(2): 253-272. (In Persian with English abstract)

Mohkamkar company, 2007. Geology and Exploration report on the Gramabe paein deposit. Geological Survey of Iran, Semnan, 180 pp.

Monazami. B.R., 1994. Genesis of Mn Mineralization in the Darab area (Fars province, Iran). M.Sc. Thesis, Shiraz University, Shiraz, Iran, 180 pp. (in Persian with English abstract)

Mousivand, F., 2003. Mineralogy, geochemistry and genesis of copper mineralization in the Surian volcani-sedimentary complex in the Bavanat area, Fars Province-Unpubl. M.Sc. thesis, Tarbiat Modarres University, Tehran, Iran, 300 pp. (in Persian with English abstract)

Mousivand, F., 2010. Geology, geochemistry and genesis of the Chahgaz Zn–Pb–Cu deposit, south of Shahre Babak; and its comparison with the Bavanat Cu–Zn–Ag volcanogenic massive sulfidedeposit, in the south Sanandaj–Sirjan zone. Ph.D. thesis, Tarbiat Modares University, Tehran, Iran, 505 pp. (in Persian with English abstract)

Mousivand, F., Rastad, E. and Emami, M.H., 2004. Bavanat copper deposit; a Besshi-type volcanogenic massive sulfide deposit in Iran. 22nd Annual Symposium of Geosciences, Geological Survey of Iran, Tehran, Iran. (in Persian with English abstract)

Mousivand, F., Rastad, E., Hoshino, K. and Watanabe, M., 2007. The Bavanat Cu- Zn- Ag orebody,First rcognition of a Besshi- type VMS deposit in Iran. Journal of Mineralogy and Geochemistry, 183(3): 297- 315.

Mousivand, F., Rastad, E. and Peter, J.M., 2008. An overview of volcanogenic massive sulfide deposits of Iran. 33rd International Geology Congress Oslo, Oslo, Norway.

Nazari, M., 1991. Mineralogy and Genesis of Barit doureh kashan deposit. M.sc. Thesis, Tarbiat Moallem University, Tehran, Iran, 200 pp. (in Persian with English abstract)

Ohmoto, H., 1996. Formation of volcanogenic massive sulfide deposits, the Kuroko perspective. Journal of Ore Geology Reviews, 10(3): 135-177.

Peter, J.M. and Scott, S.D., 1999. Windy Craggy, Northwestern British Columbia: the world largest Besshi- type deposit in Barrie. In: C. Turcker Barrie and M.D. Hannington (Editors), Volcanic-associated massive sulfide deposits: processes and examples in modern and ancient settings. Geological association of Canada, Ontario, pp. 261-295.

Piercey, S., 2011. The setting, style, and role of magmatism in the formation of volcanogenic massive sulfide deposits. Journal of Mineralium Deposita, 46(5): 449-471.

Rossetti, F., Nasrabady, M., Vignaroli, G., Theye, T., Gerdes, A., Razavi, M. and MoinVaziri, H., 2010. Early Cretaceous migmatitic mafic granulites from the Sabzevar range (NE Iran): implications for the closure of the Mesozoic peri- Tethyan oceans in central Iran. Journal of Terra Nova, 22(1): 26-34.

Solomon, M., 2008. Brine pool deposition for the Zn-Pb-Cu massive sulfide deposits of the Bathurst minig camp, New Brunswick, Canada, Comparisons with the Iberian pyrite belt. Journal of Ore Geology Reviews, 33(4): 329-351.

Sun, S.S. and Mcdonough, W.F., 1989. Chemical and isotopic systematics of oceanic basalts; implications for mantle composition and processes. In: A.D. Saunders and M.J. Norry (Editors), Magmatism in the oceanic basins. Geological Society of London, London, pp. 313-345.

Tashi, M., Mousivand, F. and Ghasemi, H., 2014. Volcanogenic massive sulfide Cu-Ag mineralization in the Kharturan area, southeast of Shahrood. 1th International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Silk Road Higher Education Cooperation Forum, China University of Geosciences (Wuhan), Wuhan, China.

Tornos, F., 2006. Environment of formation and styles of volcanogenic massive sulfides: The Iberian Pyrite Belt. Journal of Ore Geology Reviews, 28(3): 259-307.

Vahdati Daneshmand, F. and Saeidi, A., 1997. Geological map of Darin, scale 1:100,000. Geological Survey of Iran.

Whitney, D.L. and Evans, B.W., 2010. Abbreviations for names of rock-forming minerals. American Mineralogist, 95(1): 185-187.

Yarmohammadi, A., Rastad, E., Mousivand, F. and Watanabe, M., 2008. Barika Au–Ag–(Zn–Pb–Cu) deposit: First recognition of gold-rich Kuroko-type VMS mineralization in Iran. 33rd International Geology Congress Oslo, Oslo, Norway.