نتایج جستجو برای: gold ore treatment

تعداد نتایج: 1476695  

Journal: :Journal of Geography (Chigaku Zasshi) 1950

Abedini, Ali, Aliyari, Farhang, Calagari, AliAsghar, Yousefi, Tohid,

The Zarshuran Carlin-type gold deposit is located about 30 km north of Takab, West-Azarbaidjan Province, NW Iran. Interaction between the ore-forming fluids and the host carbonates and shales resulted in development of the decarbonatization, argillic, alunite, silicic, and sulfide alteration zones in the study area. Based on mesoscopic and microscopic studies on drill core samples, gold mineral...

2014
N. Dhawan

The drum agglomeration of nickel laterite and gold ores has been optimized through the design of experiments (DOE) using a Taguchi L16 (45) orthogonal array to determine the optimum conditions for maximizing average agglomerate size and minimizing the amount of fines. The effects of controllable operating factors including moisture content (nickel laterite ore: 34-37%; gold ore: 7-10%), retenti...

2010
Lesley Andrews

Some idea of the possibilities of microbeam techniques can be illustrated by examining the following example of a run of mine gold ore sample. Milling and bulk chemical analysis of the ore will provide major and minor element analysis as well as the gold grade. More detailed chemistlY can also reveal the presence of trace elements that may be advantageous or deleterious to downstream processing...

Journal: :زمین شناسی اقتصادی 0
رضوان مهوری رضا شمسی پور دهکردی هاشم باقری موسی نقره ئیان محمد علی مکی زاده

kalchoye copper-gold deposit is located about 110 kilometers east of esfahan province and within the eocene volcano sedimentary rocks. sandy tuff and andesite lava are important members of this complex.the form of mineralization in area is vein and veinlet and quartz as the main gangue phase. the main ore minerals are chalcopyrite, chalcocite, galena and weathered minerals such as goethite, iro...

2010
S. S. Dimov

An increasing number of low-grade gold ore deposits are characterized by the presence of gold as solid solution into the mineral matrix of sulphide minerals which is not directly amenable to gold cyanidation. In order to liberate this submicroscopic gold the ore has to be oxidized before being subjected to gold cyanidation and exctraction. This is mainly done by autoclave pressure oxidation (AC...

I. Rassa K. Shabani M. Momenzadeh N. Nezafati

The Tareek Darreh gold deposit is located 40km north of Torbat-e Jaam in the Khorassan-Razavi province, NE-Iran. The study area mainly comprises slightly metamorphosed, sedimentary rocks of Jurassic age including alternation of shale, siltstone, and sandstone. These rocks have been intruded by plutonic rocks such as gabbro-norite, diorite, quartz-diorite, and rhyodacite. The ore bodes are expos...

2014
Anshul Thakur G. Kalaimagal

This paper presents a feasibility study of a wearable helmet in order to protect mine workers specially of goldmines from carbon monoxide poisoning and cyanidation. Carbon monoxide(CO) poisoning is a common problem faced by the workers of coal, gold and many other mines. On the other hand cyanidation problem occurs in gold mines only during ore processing. Current safety systems for mine worker...

Calagari, , Hassani Soughi, , Sohrabi, ,

The gold-bearing prospect area at Gharehchay is located in about 2 km south of Tikmehdash, East-Azarbaidjan, NW Iran. The host rocks of the gold-bearing quartz veins/veinlets are principally Eocene andesites and upper Eocene-Oligocene felsic intrusive body (granite to alkali granite). Wall rocks alteration haloes developed around the veins/veinlets are mainly of silicic, phyllic, phyllic-argill...

Journal: :فیزیک زمین و فضا 0
محمدرضا حیدریان شهری دانشگاه فردوسی مشهد- دانشیار محمدحسن کریم پور دانشگاه فردوسی مشهد- استاد آزاده ملک زاده دانشگاه فردوسی مشهد- دانشجوی دکتری

hired is a large gold prospecting area which is located in south khorasan province, in the east of iran. gold mineralization is found in 4 target areas covering about 24 km2. the host rocks are mainly tertiary volcanics, some jurassic and cretaceous sediments. sub-volcanic rocks are of magnetite series (gabbros to diorite) and ilmenite series (granite-granodiorite-monzonite) which have intruded...

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