Investigation of cu vein of the Shurk and associated gossan zone (North West of Birjand) based on alteration, mineralization, geochemistry and fluid inclusion

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JAVIDI MOGHADDAM MARYAM; KARIMPOUR MOHAMMAD HASSAN; MALEKZADEH SHAFAROUDI AZADEH

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Journal: ADVANCED APPLIED GEOLOGY Year:2019 | Volume:9 | Issue:3 (33) Page(s): 316-340

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Title

Investigation of cu vein of the Shurk and associated gossan zone (North West of Birjand) based on alteration, mineralization, geochemistry and fluid inclusion

Author(s)

JAVIDI MOGHADDAM MARYAM | KARIMPOUR MOHAMMAD HASSAN | MALEKZADEH SHAFAROUDI AZADEH | Issue Writer Certificate

Keywords

MineralizationQ2

Fluid inclusionQ1

MixingQ1

EpithermalQ1

ShurkQ1

Abstract

1-Introduction Recent studies concerning fluid evolution in magmatic-hydrothermal systems have mainly concentrated on porphyry copper and Epithermal high-sulfidation Au-(Ag) deposits (Bethke et al., 2005; Einaudi et al., 2003; Fifarek and Rye, 2005; Heinrich, 2005). In contrast, less attention has been paid to associated Epithermal base metal deposits which occur in the upper parts of the same environment and form later in the evolution of the system than the precious metal deposits (Baumgartner and Fontboté , 2008). The Shurk area is in the west of the Lut Block volcanic– plutonic belt, in eastern Iran, about 125 Km northwest of Birjand city. Great Tertiary, The Shurk area, is located in the west of the Lut Block volcanic– plutonic belt, in eastern Iran, about 125 Km northwest of Birjand city. The Tertiary magmatic activity in the Lut Block is spatially and temporally associated with several types of Mineralization events (Karimpour et al., 2012). The prospecting area covers a significant part of the Lut Block that includes numerous cases of Cu± Pb± Zn vein-type Mineralization, such as Shikasteh Sabz, Mir-e-Khash, Rashidi, Ghar-e-Kaftar, Howz-e-Dagh (Lotfi, 1982), as well as kaolin deposit (Cheshmeh Khuri area) in the neighboring area. Mineralization in the Shurk district generally described by Lotfi (1982) and Tarkian et al. (1983). Any author has published no minutiae study regarding fluid evolution and ore genesis at the Shurk district. We present and discuss geology, alteration, ore petrography, geochemistry, and Fluid inclusion microthermometry, which help clarify the ore genesis of the Shurk area...

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APA: Copy

JAVIDI MOGHADDAM, MARYAM, KARIMPOUR, MOHAMMAD HASSAN, & MALEKZADEH SHAFAROUDI, AZADEH. (2019). Investigation of cu vein of the Shurk and associated gossan zone (North West of Birjand) based on alteration, mineralization, geochemistry and fluid inclusion. ADVANCED APPLIED GEOLOGY, 9(3 (33) ), 316-340. SID. https://sid.ir/paper/364266/en

Vancouver: Copy

JAVIDI MOGHADDAM MARYAM, KARIMPOUR MOHAMMAD HASSAN, MALEKZADEH SHAFAROUDI AZADEH. Investigation of cu vein of the Shurk and associated gossan zone (North West of Birjand) based on alteration, mineralization, geochemistry and fluid inclusion. ADVANCED APPLIED GEOLOGY[Internet]. 2019;9(3 (33) ):316-340. Available from: https://sid.ir/paper/364266/en

IEEE: Copy

MARYAM JAVIDI MOGHADDAM, MOHAMMAD HASSAN KARIMPOUR, and AZADEH MALEKZADEH SHAFAROUDI, “Investigation of cu vein of the Shurk and associated gossan zone (North West of Birjand) based on alteration, mineralization, geochemistry and fluid inclusion,” ADVANCED APPLIED GEOLOGY, vol. 9, no. 3 (33) , pp. 316–340, 2019, [Online]. Available: https://sid.ir/paper/364266/en

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