GEOLOGY, ALTERATION, MINERALIZATION AND GEOCHEMISTRY AT SOUTH OF ARGHASH (NEYSHABOUR)

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KARIMI Z.; MAZAHERI S.A.; KARIMPOUR M.H.

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

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Journal: JOURNAL OF ECONOMIC GEOLOGY Year:2011 | Volume:2 | Issue:2 Page(s): 167-189

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Title

GEOLOGY, ALTERATION, MINERALIZATION AND GEOCHEMISTRY AT SOUTH OF ARGHASH (NEYSHABOUR)

Author(s)

KARIMI Z. | MAZAHERI S.A. | KARIMPOUR M.H. | Issue Writer Certificate

Keywords

RESEARCH CENTER FOR ORE DEPOSITS OF EASTERN IRANQ2

FERDOWSI UNIVERSITY OF MASHHADQ2

Abstract

The Arghash area is located 45 km to southwest of Neyshabour. The sub volcanic rocks in the area consist of biotite hornblende quartz monzodiorite porphyry, hornblende biotite quartz monzodiorite porphyry, hornblende monzonite porphyry, biotite hornblende monzonite porphyry, monzodiorite porphyry and biotite quartz monzodiorite porphyry units. The volcanic rocks consist of hornblende biotite dacite, biotite hornblende dacite, and andesite and pillow lava. The plutonic rocks consist of hornblende monzodiorite, hornblende monzonite, quartz monzonite, hornblende quartz monzodiorite, biotite granodiorite, hornblende granodiorite, biotite hornblende granodiorite, biotite quartz diorite and pyroxene dolerite units. Five types of alteration including propylitic, carbonate, argillic, silicification and sericitic were recognized. Those are subdivided into twelve sub-zones based on the mineral abundances and intensity of alteration. Primary pyrite, 3-4%, is found mainly as disseminated. Secondary mineralization includes limonite, hematite and jarosite. Twenty rock chip and 8 stream sediment samples were collected for geochemical exploration. The samples were analysed for Cu, Zn, Pb, Ag and Sb using Atomic Absorbtion Spectrophotometric (AAS) method. In stream sediment samples, Cu abundance is 34-58 ppm, Zn 45-422 ppm, Pb 28-42 ppm and Ag 2-12 ppm, whereas in rock chip samples, Cu abundance is 8-1137 ppm, Zn 13-411 ppm, Pb 15-97 ppm and Ag 3-32 ppm.

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References

ویژگی های پترولوژیکی و کانه زایی در گرانیتوئیدهای فردوس (همایش)

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APA: Copy

KARIMI, Z., MAZAHERI, S.A., & KARIMPOUR, M.H.. (2011). GEOLOGY, ALTERATION, MINERALIZATION AND GEOCHEMISTRY AT SOUTH OF ARGHASH (NEYSHABOUR). JOURNAL OF ECONOMIC GEOLOGY, 2(2), 167-189. SID. https://sid.ir/paper/180477/en

Vancouver: Copy

KARIMI Z., MAZAHERI S.A., KARIMPOUR M.H.. GEOLOGY, ALTERATION, MINERALIZATION AND GEOCHEMISTRY AT SOUTH OF ARGHASH (NEYSHABOUR). JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2011;2(2):167-189. Available from: https://sid.ir/paper/180477/en

IEEE: Copy

Z. KARIMI, S.A. MAZAHERI, and M.H. KARIMPOUR, “GEOLOGY, ALTERATION, MINERALIZATION AND GEOCHEMISTRY AT SOUTH OF ARGHASH (NEYSHABOUR),” JOURNAL OF ECONOMIC GEOLOGY, vol. 2, no. 2, pp. 167–189, 2011, [Online]. Available: https://sid.ir/paper/180477/en

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