نتایج جستجو برای: chalcocite

تعداد نتایج: 143  

Mazloumi Bajestani, , Malekzadeh Shafaroudi, , Sahebi Khader, ,

Fadiheh copper-gold prospect area in northwest of Torbat-e Heydariyeh in Khorasan Razavi Province is located in the central part of the Khaf-Kashmar-Bardaskan magmatic belt. This area includes outcrops of Eocene volcanic-pyroclastic units with felsicـintermediate nature. The lavas are andesite and latite, and pyroclastic units include rhyodacitic tuff, andesitic lithic tuff and ignimbrite. Intr...

Onzon-Kanbani area is a western flank of Mogok Metamorphic Belt where gold mineralization is hosted as auriferous quartz-vein with epithermal low-sulphidation characters. Mineralization is closely associated with NE-SW trending fracture or shear zone probably related to the dextral movement of the Sagaing Fault system. Mineralization related hydrothermal alteration is developed as narrow zones ...

Journal: :زمین شناسی اقتصادی 0
قاسم نباتیان مجید قادری نعمت اله رشیدنژاد عمران فرحناز دلیران

sorkheh-dizaj apatite-iron oxide deposit is located 32 km southeast of zanjan. the area is situated within the tarom subzone of western alborz-azarbaijan structural zone. the oldest units at the sorkheh-dizaj area are eocene trachyte, trachyandesite, olivine basalt and volcanoclastic brecciate tuff and lapilli tuff which intruded by a quartz-monzonite, monzonite and granite subvolcanic pluton o...

Journal: :زمین شناسی اقتصادی 0
علیرضا زراسوندی فاطمه اسدی هوشنگ پورکاسب فرهاد احمدنژاد حسن زمانیان

introduction a wide variety of world-class porphyry cu deposits occur in the urumieh-dohktar magmatic arc (udma) of iran.the arc is composed of calc-alkaline granitoid rocks, and the ore-hosting porphyry intrusions are dominantly granodiorite to quartz-monzonite (zarasvandi et al., 2015). it is believed that faults played an important role in the emplacement of intrusions and subsequentporphyry...

Journal: :زمین شناسی اقتصادی 0
سلیمه سادات کمیلی محمود خلیلی هوشنگ اسدی هارونی هاشم باقری فریماه آیتی

introduction the kahang cu- mo deposit is situated approximately 73 km northeast of isfahan. asadi (2007) identified a geological reserve of 40 mt (proven reserve) grading at 0.53 cu, 0.02 mo and estimated reserve of 120 mt. all the rock types in the region have been subjected to hydrothermal solutions which gave rise to three different alteration facies. the dacite and rhyodacite volcanic rock...

Gholami, , Karimpour, , Malekzadeh Shafaroudi, ,

Sangan prospect area is located northeast of Torbat-e-Heydarieh in Khorasan Razavi Province and in relation to regional geology, it is situated in eastern section of Khaf-Kashmar-Bardaskan magmatic belt. Metamorphosed sediments of the Shemshak Formation (slate, schist, quartzite) is the oldest unit, which is intruded by Kafardoogh granitic intrusion. The dikes of quartz monzosyenitic and diorit...

احمدی خلجی, احمد, حسین زاده, محمدرضا, رادمرد, کیخسرو, زمانیان, حسن,

The Mazra'eh Shadi is located about 130 km northeast of Tabriz (NW Iran) in the Arasbaran metallogenic belt. The deposit occurs as a series of veins within the Eocene andesites. Mineralization shows epithermal system that controlled by fault distribution. Epithermal textures within the veins include comb, vaggy quartz, cockade, boxworke, plate calcite and breccia. Pyrite is the main ore mineral...

2006
M. D. HANNINGTON P. STOFFERS I. C. WRIGHT A. G. REYES E. T. BAKER G. J. MASSOTH J. E. LUPTON R. R. GREENE C. W. R. SOONG J. ISHIBASHI G. T. LEBON C. J. BRAY J. A. RESING

Brothers volcano, which is part of the active Kermadec arc, northeast of New Zealand, forms an elongate edifice 13 km long by 8 km across that strikes northwest-southeast. The volcano has a caldera with a basal diameter of ~3 km and a floor at 1,850 m below sea level, surrounded by 290to 530-m-high walls. A volcanic cone of dacite rises 350 m from the caldera floor and partially coalesces with ...

Journal: :زمین شناسی اقتصادی 0
منصور عادل پور ایرج رساء فریبرز مسعودی مسعود حسینی

introduction the garmab copper deposit is located northeast of qaen (south khorasan province) in the1:100,000 scale map of abiz in the eastern tectonic zone of iran. it is hosted by late paleocene-eocene lava flows consisting mainly of andesite, trachy andesite, andesite-basalt and basalt lavas, as well as pyroclastic rocks, including tuffs and ignimbrites. the lut block has undergone intense m...

ژورنال: :پژوهش های دانش زمین 0
مریم قربان کهریزسنگی دانشگاه شهید بهشتی سعید علیرضایی دانشگاه شهید بهشتی هوشنگ اسدی هارونی دانشگاه صنعتی اصفهان

کانسار مس- طلای کالچویه، در 25 کیلومتری شرق شهرستان کوهپایه در استان اصفهان قرار دارد. این ناحیه در بخش جنوب شرقی ورقه 100000/1 کجان و در بخش میانی کمان ماگمایی ارومیه-دختر واقع شده است. داده های دورسنجی بر اساس شناسایی دگرسانی ها، نشانگر چند آنومالی است که برخی با کانی سازی همراه است. کانی سازی در کالچویه در قالب دو رگه کوارتز به همراه کانی های سولفیدی است. رگه اصلی با امتداد n40e، دارای طول ح...

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