GEOCHEMISTRY AND PETROLOGY OF TANURJEH PORPHYRY AU-CU MINERALIZED SYSTEM

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KARIMPOUR M.H.; SAADAT S.; MALEKZADEH SHAFAROUDI A.

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Journal Paper

Paper Information

Journal: JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT) Year:2006 | Volume:32 | Issue:3 (SECTION GEOLOGY 2) Page(s): 175-187

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Information Journal Paper

Title

GEOCHEMISTRY AND PETROLOGY OF TANURJEH PORPHYRY AU-CU MINERALIZED SYSTEM

Author(s)

KARIMPOUR M.H. | SAADAT S. | MALEKZADEH SHAFAROUDI A. | Issue Writer Certificate

Keywords

PORPHYRY GOLDQ3

PYRITEQ3

TANURJEHQ3

IRANQ3

Abstract

The TANURJEH area is located in the Khaf-Darouneh volcano-plutonic belt, North of Darouneh Great fault. Eocene "Volcanicrocks such as rhyolite, dacite, rhyodacite and minor andesite are present. They are found mainly as tuff, lapilli tuff and flow. 19 sub volcanic (Oligo-Miocene) bodies with composition of monzonite, quartz monzonite, diorite and quartz diorite porphyry are mapped. Different types of alteration such as propylitic, solidification with vugs, sericitic are well developed in the area. Silicified zone cover a large area. Alteration zones are not linear and it is inferred that they are formed due to sub-volcanic intrusive. PYRITE and minor chalcopyrite are the main primary sulfides. They occur both as dissemination and fracture filling. In most of the areas, sulfides are oxidized. Secondary oxides are between 0.3 8 percent. Au, Cu, Zn, Pb, As, and Mo show anomaly in the area The Au content of rock samples are between 0.1 11.2 ppm. TANURJEH has several features analogous to gold-rich porphyry deposits: cluster of sub-volcanic intermediate calcalkaline rocks, hydrothermal alteration closely associated with the intrusive bodies, present of gold anomaly in most of the area, extensive solidification. (vuggy quartz) is dominate, and presence of PYRITE, mostly oxidized, both disseminated and veinlets.

Cites

PETRO GENESIS OF GRANITOIDS, U-PB ZIRCON GEOCHRONOLOGY, SR-ND PETRO GENESIS OF GRANITOIDS, U-PB ZIRCON GEOCHRONOLOGY, SR-ND ISOTOPIC CHARACTERISTICS, AND IMPORTANT OCCURRENCE OF TERTIARY MINERALIZATION WITHIN THE LUT BLOCK, EASTERN IRAN

References

استفاده از Rb/Sr، Sm/Eu و Ce/Yb برای تشخیص گرانیت های تیپ با کانی سازی قلع و بدون کانی سازی قلع

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APA: Copy

KARIMPOUR, M.H., SAADAT, S., & MALEKZADEH SHAFAROUDI, A.. (2006). GEOCHEMISTRY AND PETROLOGY OF TANURJEH PORPHYRY AU-CU MINERALIZED SYSTEM. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 32(3 (SECTION GEOLOGY 2)), 175-187. SID. https://sid.ir/paper/2285/en

Vancouver: Copy

KARIMPOUR M.H., SAADAT S., MALEKZADEH SHAFAROUDI A.. GEOCHEMISTRY AND PETROLOGY OF TANURJEH PORPHYRY AU-CU MINERALIZED SYSTEM. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2006;32(3 (SECTION GEOLOGY 2)):175-187. Available from: https://sid.ir/paper/2285/en

IEEE: Copy

M.H. KARIMPOUR, S. SAADAT, and A. MALEKZADEH SHAFAROUDI, “GEOCHEMISTRY AND PETROLOGY OF TANURJEH PORPHYRY AU-CU MINERALIZED SYSTEM,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 32, no. 3 (SECTION GEOLOGY 2), pp. 175–187, 2006, [Online]. Available: https://sid.ir/paper/2285/en

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