نتایج جستجو برای: sulfidic mineralized zones

تعداد نتایج: 49927  

H Ranjbar

The northwestern part of the Kerman Cenozoic magmatic arc (KCMA) contains many areas with porphyry copper mineralization. In this research, we used the advanced space-borne thermal emission and reflection radiometer (ASTER) and Enhanced Thematic Mapper plus (ETM+) images of this region to map the distribution of hydrothermally altered rocks, based on their mineral assemblages. The spectral meas...

Journal: :Applied earth science 2021

Proterozoic limestone in a north British terrane contains newly recognised occurrence of Nb-REE minerals. The mineralized Loch Shin Limestone is the Lewisian Complex Northern Highlands Scotland, intruded by alkaline plutons above Caledonian (∼0.43 Ga) subduction zone. mineral assemblage includes columbite, calcium niobate minerals, and niobian rutile also W- Sn-bearing phases. interval between ...

Journal: Geopersia 2012
Hassan Mirnejad Soheila Nourali

Sar-Kuh porphyry copper deposit is located 6 km southwest of the Sar-Cheshmeh copper mine, Kerman Province, Iran. Based on field geology, petrography and fluid inclusions studies, four alteration types have been identified in the Sar-Kuh area. Early hydrothermal alteration formed a potassic zone in the central parts of Mamzar granite/grano-diorite stock and propylitic alteration in its peripher...

Ghalmaghash, , Hasanzadeh,, , Heidari, , Mohebi, ,

Zavarian epitermal gold (copper) deposit is located in an intracontinental volcanic cone (stratovolcano) with the Early Miocene age, in the middle of the Urmia-Dokhtar magmatic arc. The host rocks of this mineralization include a set of basaltic, andesitic-basaltic, andesitic, dacitic, as well as granodiorite and tonal units that have been exposed in volcanic form (lava and pyroclastic) and sem...

2009
Alexandra Stock Klaus Jürgens John Bunge Thorsten Stoeck

The Gotland Deep is a temporary anoxic basin in the central Baltic Sea that is frequently subjected to inflow events which result in oxygenation of the deep water. We examined the protistan community structure in this environment several months after such an inflow event by analyzing small subunit ribosomal RNA (18S rRNA) sequences from samples collected in the oxic–anoxic transition zone (200 ...

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...

2011
Virginia P. Edgcomb Edward R. Leadbetter William Bourland David Beaudoin Joan M. Bernhard

Marine micro-oxic to sulfidic environments are sites of intensive biogeochemical cycling and elemental sequestration, where prokaryotes are major driving forces mediating carbon, nitrogen, sulfur, phosphorus, and metal cycles, important from both biogeochemical and evolutionary perspectives. Associations between single-celled eukaryotes and bacteria and/or archaea are common in such habitats. H...

Journal: :Journal of trace elements in medicine and biology : organ of the Society for Minerals and Trace Elements 2012
Dirk Schaumlöffel

This review gives an overview on the analysis of inorganic nickel species and their toxic effects. Based on the analytical procedure applied inorganic nickel species are usually classified in soluble, sulfidic, metallic and oxidic nickel fractions. Only few works were attempting a chemical characterization of the different nickel compounds in each fraction. This general classification in four n...

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