Mineralogy and Formation Conditions of Turquoise in Ali Abad Cu Porphyry Deposit

زمین شناسی اقتصادی

Article 5, Volume 12, Issue 1 - Serial Number 24, 2020, Pages 93-109   

Document Type: Research Article

DOI: 10.22067/econg.v12i1.72122

Authors

Saeide Jadidi Ardekani¹; Mohammad Ali Mackizadeh^{* 1}; Farimah Ayati²

¹University of Isfahan

²Payame Noor University

Abstract

Introduction
In porphyry copper deposits, turquoise is considered to be a supergene oxidation product (John et al., 2010; Chavez, 2000). Based on Rezaian et al., 2003; Zarasvandi et al., 2005 and Eslamizadeh, 2004, the Aliabad index is introduced as a porphyry copper system. The first published report on turquoise events around Ali-Abad was presented by Momenzadeh et al., 1988. This area is located 57 km southwest of Yazd. Alterations often include siricitization, advanced argillization. Kaolinization and silicification have occurred frequently in the arkose and microcan glomerate of the Sangestan formation. The aim of this research study is to try to reconstruct and investigate the formation and origin of turquoise by using the latest mineralogical and geochemical data. Field evidence shows occurrence of turquoise in the form of a veinlet and nodules, with blue-green and blue-white colors. Jarosite, alunite, quartz and iron oxides are found together with turquoise.
 
Materials and Methods
A geological map of the area with a scale of 1/15000 was prepared. 35 samples of intrusive bodies, sandstones and altered rocks were selected to produce thin and polished sections. XRD and the EDS analyses were carried out at the central laboratory of Isfahan University and the University of Oklahoma, USA, respectively in order to identify the chemical composition of phases.
Results
Based on the studies, several chain processes have been involved in the form of turquoise: the initiator of the reactions is the formation of an oxidant environment (gossan), in which metal sulfides (Cu, Fe) in the phyllic zone of porphyry copper deposit have played a fundamental role. Turquoise has two species in this area. One is in the form of direct deposition in the veinlets, away from the alteration of the host rock and the mineralization center, and the other one is in the form of substitution. It is undeniable that the host rock with Kaolinite-sericite alteration is required for substitution. The close association of alunite-turquoise may imply that turquoise is a product of the phosphatization process of alunite. The Alunite Supergene event in the alteration zone and its accompaniment with turquoise indicates the mineral complex of advanced argillic alteration. The mineral chemistry highlighted the high percentages of aluminum concentration which is a property of minerals in advanced argillic zone.
 
Discussion
The phyllic zone has the largest part of the region's alteration (Taghipour and Mackizadeh, 2011; Moore et al., 2011). An advanced argillic zone with the presence of alunite-jarosite with turquoise is scattered inside the phyllic zone. To confirm microscopic observations, XRD and EDS analyses were used. These analyses prove the presence of the turquoise phase.
In some analyses performed on the turquoise mineral phase, the presence of potassium and silicon probably indicates the transitional phase of conversion of sericite or alunite to turquoise. Pyrite in the oxidant condition has been disrupted by the effects of atmospheric water and created goethite and sulfuric acid. The produced ferric sulfate can induce dissolution of chalcopyrite. The occurrence of iron oxides and oxy-hydroxides will lead to the development of the gossan zone. Gossan's transformation, in addition to supplying copper, causes acidic fluids to continue the reaction. Under acidic conditions, the phosphate leaching from the arkose has been subjected to the following reaction:
Ca5 (PO4)3OH + 5H2SO4 + 9/2O2 → 5CaSO4 2H2O + 3H3PO4
In addition to phosphate and copper, aluminum is the most important element in the structure of turquoise. Under an acidic environment, arkose feldspars and hydrolysis reactions during alteration will be used for the formation of sericite, kaolinite and gypsite. With the presence of sulfate and potassium released from the alteration of feldspars, alunite and turquoise can be formed. The alunite-turquoise paragenesis confirms formation of turquoise by alunite (Espahbod, 1976). Turquoise will be formed by the reaction of potassium, copper sulfate and anion phosphate with alunite:
8K+ + CuSO4 + 4H2PO4- + 2KAl3 (SO4)2(OH) 6 → CuAl6 (PO4)4(OH)8 4H2O + 5K2SO4 + 4H+
The hydrogen ions released in this reaction will lower the pH of the environment and cause progression of hydrolysis reactions. Finally, jarosite will be formed by the interaction of K+, sulfate and Fe3+. Based on these reactions, an aluminum-rich phase is needed for stabilizing phosphate and soluble copper.
 
References
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Keywords

turquoise; Alunite; cu-porphyry; Aliabad; Central Iran

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