Geology, alteration, mineralization, petrogenesis, geochronology, geochemistry and airborne geophysics of Kuh Shah prospecting area, SW Birjand

Document Type : Research Article

Authors

Ferdowsi University of Mashhad

Abstract

The Kuh Shah prospecting area is located in Tertiary volcano-plutonic belt of the Lut Block. More than seventeen subvolcanic intermediate to acidic intrusive rocks, diorite to syenite in composition, were identified in the study area. The intrusions are related to hydrothermal alteration zones and contain argillic, propylitic, advanced argillic, silicified, quartz-sericite-pyrite, gossan and hydrothermal breccia which overprinted to each other and are accompanied by weathering which made it complicated to distinguish zoning. Mineralization is observed as sulfide (pyrite and rare chalcopyrite), disseminated Fe-oxides and quartz-Fe-oxide stockwork veinlets. Intrusive rocks are metaluminous, calc-alkaline with shoshonitic affinity with high values of magnetic susceptibility. The Kuh Shah intrusive rocks are classified as magnetite-series of oxidant I-type granitoids. Based on zircon U–Pb age dating, the age of these granitoid rocks is 39.7± 0.7 Ma (Middle Eocene). The radioisotope data (initial 87Sr/86Sr and 143Nd/144Nd ratios as well as εNd) and geochemical data suggest that the Kuh Shah granitoid rocks formed from depleted mantle in a subduction-related magmatic arc setting. Geochemical anomalies of elements such as Cu, Au, Fe, Pb, Zn, As, Sb, Mo, Bi, Hg and also Mn, Ba, Te and Se, correlated with quartz-sericite-pyrite, gossan-stockwork-hydrothermal breccias, irregular silicified bodies and advanced argillic hydrothermal alteration zones. Geophysical anomalies correlated with hydrothermal alteration and mineralization zones. The interpretation of the results represents complex patterns of sub-circular to ellipsoid shape with north-east to south-west direction. These evidences are similar to the other for known Cu-Au porphyry and Au-epithermal systems in Iran and worldwide.

Keywords


[1] Eftekhar-Nezhad J., "Birjand 1:250000 geological quadrangle map", Geological Survey of Iran (1990).
[2] Eftekhar-Nezhad J., Stocklin J., Movahed-e-Avval H., Emami M.H., "Mokhtaran Geological Map, scale 1:100000, Sheet 7854", Geological Survey of Iran (1978).
[3] آقانباتی ع.، "زمین شناسی ایران"، سازمان زمین شناسی و اکتشافات معدنی کشور، (1383) 586 ص.
[4] کریم پور م. ح.، ملکزاده شفارودی آ.، مظاهری س. ا.، حیدریان م. ر.، "ماگماتیزم و انواع کانی سازی مس، طلا، قلع و تنگستن در بلوک لوت"، پانزدهمین همایش انجمن بلورشناسی و کانی شناسی ایران، دانشگاه فردوسی مشهد، (1386).
[5] Adams S. S., "Using Geological Information to Develop Exploration Strategies For Epithermal Deposits", Reviews in Economic Geology, 2 (1985) 273-298.
[6] Sillitoe R. H., "Epithermal models: Genetic types, geometrical controls and shallow features", Geological Association of Canada, Special Paper, 40 (1993) 403–417.
[7] Sillitoe R. H., "Exploration of porphyry copper lithocaps", In: Mauk J. L., St George J.D., (eds) Proc Pacrim Congress 95, Auckland 1995, Australas Inst Mining Metall Publ Ser 9/95 (1995) 527-532.
[8] Sillitoe R. H., Steele G. B., Thompson J. F. H., Lang J. R., "Advanced argillic lithocaps in the Bolivian tin-silver belt", Mineralium Deposita, 33 (1998) 539-546.
[9] Middlemost E. A. K., "Magmas and magmatic rocks", Longman, London & New York (1985) 266 p.
[10] Rickwood P. C., "Boundary lines within petrologic diagrams which use oxides of major and minor elements", Lithos 22 (1989) 247–267.
[11] Irvine T. N., Baragar W. R. A., "A guide to the chemical classification of the common volcanic rocks", Canadian Journal of Earth Sciences 8 (1971) 523–548.
[12] Whalen J. B., Currie K. L., Chappell B. W., "A-type granites: geochemical characteristics, discrimination and petrogenesis", Contributions to Mineralogy and Petrology 95 (1987) 407–419.
[13] Shand S. J., "Eruptive rocks; Their genesis, composition, classification and their relation to ore-deposits", Hafner Publishing Co., New York (1947) 488 p.
[14] Pearce J. A., Harris N. B. W., Tindle A. G., "Trace element discrimination diagrams for the tectonic interpretation of granitic rocks", Journal of Petrology 25 (1984) 956-983.
[15] Condie K. C., "Geochemical changes in basalts and andesites across the Archean–Proterozoic boundary: identification and significance", Lithos 23 (1989) 1–18.
[16] Brown G. C., Thorpe R. S., Webb P. C., "The geochemical characteristics of granitoids in contrasting arcs and comments on magma sources", Journal of Geological Society of London 141 (1984) 413–426.
[17] Martin H., "The Archaean grey gneisses and the genesis of the continental crust. In: Condie K.C. (Ed.), The Archaean Crustal Evolution", Elsevier, Amsterdam (1993).
[18] Pearce J. A., "Role of sub-continental lithosphere in magma genesis at active continental margins. In: Continental Basalts and Mantle Xenoliths—Hawkesworth C. J., Norry M. J., eds", Nantwich, UK: Shiva. (1983).
[19] Boynton W. V., "Cosmochemistry of the rare earth elements: meteorite studies. In: Henderson P. (Ed.), Rare Earth Element Geochemistry", Elsevier Sci Publ. Co., Amsterdam (1984).
[20] Karimpour M. H., Stern C. R., Farmer L., Saadat S., Malekezadeh A. "Review of age, Rb-Sr geochemistry and petrogenesis of Jurassic to Quaternary igneous rocks in Lut Block, Eastern Iran", Geopersia, University of Tehran, Iran 1(2011) 19-36.
[21] Gehrels G. E., Valencia V., "A Pullen in geochronology: emerging opportunities. In: T. Loszewski and W. Huff (Eds.) ", Paleontology Society, Short Course, 12 (2006) 67–76.
[22] سازمان زمین‌شناسی کشور، "گزارش اکتشافات ژئوشیمیایی سیستماتیک در برگه 100000/1 مختاران"، وزارت صنایع و معادن، (1379).
[23] سازمان زمین‌شناسی کشور، "گزارش اکتشافات ژئوشیمیایی نیمه تفصیلی محدوده آنومالی 20000/1 شیخ آباد"، وزارت صنایع و معادن، (1382).
[24] سازمان زمین شناسی و اکتشافات معدنی کشور، "پروژه ژئوفیزیک هوائی بیرجند- خوسف (استان خراسان جنوبی)"، وزارت صنایع و معادن، (1383).
[25] Dickson B. L., Fraser S. L., Kinsey-Henderson A., "Interpreting aerial gamma-ray surveys utilizing geomorphplogical and weathering models", Journal of Geochemical Exploration, 57 (1996) 75-88.
[26] Howe B., Kroll A., "The Geophysical Response of the Tupinda Cu-Au-Mo Porphyry Prospect, Tabar Islands, Papua New Guinea", ASEG, Sydney, Australia (2010).
[27] Sillitoe R., "Gold-Rich Porphyry Deposits: Descriptive and Genetic Models and Their Role in Exploration and Discovery", SEG Reviews, 13 (2000) 315-345.
[28] Sillitoe R. H., Hedenquist J. W., "Linkages between volcano-tectonic settings, ore-fluid compositions, and epithermal preciousmetal deposits", In Simmons S. F, Groham I. (eds), Volcanic, Geothermal, and ore-forming fluids: Rulers and witnesses of processes deep within the earth, Giggenbach memorial volume. Soc. Econ. Geol. Geochem. Soc. Sp.Pub. 10 (2003) 315-343.
[29] Sillitoe R., "Gold-Rich Porphyry Deposits: Descriptive and Genetic Models and Their Role in Exploration and Discovery", SEG Reviews, 13 (2000) 315-345.
[30] Ranjbar H., Shahriari H., Honarmand M., "Integration of Aster and airborne geophysical data of copper mineralization. A case study of Sar Ccheshmeh area", International society for photogrammetry and remote sensing, Turkey, (2004).
[31] Ranjbar H., Honarmand M., "Integration and analysis of airborne geophysical and ETM+ data for exploration of porphyry type deposits in the central Iranian volcanic belt using fuzzy classification", International Journal of Remote Sensing 25 (2004) 4729-4741.
[32] Ranjbar H., Hassanzadeh H., Torabi M., Ilaghi O., "Integration and analysis of airborne geophysical data of the Darrehzar area, Kerman Province, Iran, using principal component analysis", Journal of applied geophysics 48 (2001) 33-41.
[33] Sillitoe R. H., Bonham H. F., "Volcanic Landforms and Ore Deposit", Economic Geology, 79 (1984) 1286-1298.
[34] Simmons S. F., White N. C., John D., "Geological Characteristics of Epithermal Precious and Base Metal Deposits", Society of Economic Geologists, Inc., Economic Geology 100th Anniversary (2005).
CAPTCHA Image