نتایج جستجو برای: iron mineralization

تعداد نتایج: 155127  

Journal: :Integrative biology : quantitative biosciences from nano to macro 2011
Alaa A A Aljabali Sachin N Shah Richard Evans-Gowing George P Lomonossoff David J Evans

The external surface of the plant virus Cowpea mosaic virus (CPMV) can be chemically modified with peptides that direct specific mineralization processes. Subsequent mineralization of the peptide-CPMV conjugates produces monodisperse nanoparticles of ca. 32 nm diameter coated with, for example, cobalt-platinum, iron-platinum or zinc sulfide, which cannot be readily prepared by other methods. Th...

مسعودی, فریبرز , مهرابی, بهزاد , کریمی شهرکی, بهروز ,

Jalal-Abad iron deposit is located about 38 km northwest of Zarand town in Kerman Province. It contains 200 Mt iron ore with average chemical composition of Fe = 45%, S =1.18% and P = 0.08%. Iron mineralization occurs in an Early Cambrian volcano–sedimentary sequence of Rizu series which is composed of sandy siltstone, siltstone, volcanoclastic rocks and dolomite. Small intrusive bodies of gab...

Journal: :iranian journal of earth science 0
kamal h. karim department of geology, university of sulaimani, kurdistan region, iraq nabaz r.h. aziz department of geology, university of sulaimani, kurdistan region, iraq al-bidary mayssa a.a.a department of geology,university of baghdad, iraq

the asinawa iron ore is located about 3km to the southeast of penjween town, sulaimaniya governorate, kurdistan region, northeastern iraq near the iraq-iran border. the exposed iron ore deposit is about 60 and 400m wide and long respectively. the present study is the re-study of the geology and geochemistry of the asnawan iron ore deposit  and concluded that the country rocks are consist of hor...

Journal: :زمین شناسی اقتصادی 0
محمد حسن کریم پور آزاده ملکزاده شفارودی اکبر اسفندیارپور حسن محمدنژاد

neyshabour turquoise mine is located in northwest of neyshabour, southern quchan volcanic belt. eocene andesite and dacite forming as lava and pyroclastic rocks cover most of the area. subvolcanic diorite to syenite porphyry (granitoids of magnetite series) intruded the volcanic rocks. both volcanic and subvolcanic rocks are highly altered. four types of alteration are recognized including: sil...

2017
Colleen M. Hansel Shawn G. Benner Jim Neiss Alice Dohnalkova Ravi K. Kukkadapu Scott Fendorf COLLEEN M. HANSEL SHAWN G. BENNER JIM NEISS ALICE DOHNALKOVA RAVI K. KUKKADAPU

Iron (hydr)oxides not only serve as potent sorbents and repositories for nutrients and contaminants but also provide a terminal electron acceptor for microbial respiration. The microbial reduction of Fe (hydr)oxides and the subsequent secondary solid-phase transformations will, therefore, have a profound influence on the biogeochemical cycling of Fe as well as associated metals. Here we elucida...

تقی‌پور, نادر, حاجی بهرامی, مریم, قربانی, قاسم,

Hamyerd iron deposit is located about 74 km north east of Semnan, in the Jam area. This area is situated in the northern part of Central Iran structural zone. The outcrops are Middle-Eocene volcanic and pyroclastic rocks with andesite to andesite-basalt and tuff composition, which are intruded by some intrusive bodies of monzonite to monzodiorite composition in this area. Iron mineralization is...

Journal: :AJNR. American journal of neuroradiology 1992
O B Boyko P C Burger J D Shelburne P Ingram

PURPOSE To further elucidate the nonparamagnetic effects of T1-relaxation mechanisms in MR imaging. PATIENTS AND METHODS In 12 patients with lesions having hyperintense signal on T1-weighted spin-echo MR, findings were correlated with autopsy/surgical biopsy in seven cases and/or noncontrast CT scans in 10 cases. RESULTS Eight of the 10 CT scans demonstrated hyperattenuation in the lesions,...

Journal: :Metal-Based Drugs 1998
Astrid Sigel Helmut Sigel

Microorganisms, Plants, and Animals, offers a comprehensive and timely account of this fascinating topic by 35 distinguished international authorities. In 18 stimulating chapters, this volume highlights first the biological cycling of iron in oceans, followed by accounts of the transport of iron in microorganisms, fungi, and plants, the roles and properties of siderophores, and the regulation o...

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