نتایج جستجو برای: quartz veins

تعداد نتایج: 29821  

Journal: :JOURNAL OF MINERALOGY, PETROLOGY AND ECONOMIC GEOLOGY 1995

1999
Jiří Zimák

Chlorites from (1) hydrothermal veins composed of quartz and/or carbonate that cross-cut unmetamorphosed to epizonally metamorphosed Variscan flysch sequences in the Nízký Jeseník Upland, (2) Alpine-type veins in amphibolites and gneisses of the Sobotín region, and (3) pegmatites of the Žulová massif and Strzegom-Sobótka massif were studied by chemical methods to elucidate the conditions of the...

علمدار, سیده محبوبه, رحیمی, بهنام , مظاهری, سید احمد ,

The study area is located about 30km northwest of Kashmar, southwest of Keriz village and east of Siah Kuh mine. Based on field and mineralogical studies, the rocks are mainly polutonic, sub-volcanic and volcanic, aged Eocene. The carbonate unit, with Permian age, is exposed extensivelly in the area. The mineralization in the area appears as veins, lenses, massive and dissiminated forms. Vein a...

جمالی, حمایت, مهرابی, بهزاد , یعقوب پور, عبدالمجید,

The study area is located in the east of Ahar town in Eastern Azerbaijan Province and is part of the Ahar-Arasbaran Cenozoic magmatic belt of NW Iran. The geological units of the Eocene age are volcanic rocks with andesite, latite - andesite and basaltic andesite composition. Khankandi and Useflu Oligocene intrusive bodies intruded in the volcanic rocks and caused widespread alteration and copp...

Journal: :زمین شناسی اقتصادی 0
مریم فیضی محمد ابراهیمی حسین کوهستانی میر علی اصغر مختاری

introduction the aqkand cu occurrence, 48 km north of zanjan, is located in the tarom subzone of the western alborz-azerbaijan structural zone. apart from small scale geological maps of the area, i.e., 1:250,000 geological maps of bandar-e-anzali (davies, 1977) and 1:100,000 geological maps of hashtjin (faridi and anvari, 2000) and a number of unpublished perlite exploration reports, prior to t...

بومری, محمد, مرادی, راحله, باقری, ساسان , زاهدی, اعظم ,

Shurchah antimony deposit is located in flysch zone of eastern Iran. The antimony mineralization was formed in silicic veins that hosted by highly silicified and brecciated granitoids and low-grade metamorphic rocks which are rich in phyllosilicate minerals. Stibnite is the most aboundant Sb-bearing ore mineral in the veins and is associated with pyrite, chalcopyrite, arsenopyrite and gold. Sen...

Journal: :Geodinamika i Tektonofizika 2022

The paper presents the results of detailed structural analysis and 40 Ar/ 39 Ar dating deformations in Golets Vysochaishii deposit area. geological studies showed folded-deformation sequence from large lying folds through axial-plane cleavage formation to quartz-filled fractures. syntectonic sericite yielded ages two Hercynian tectonic impulses – 340 320 Ma. This stage is characterized by earli...

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