نتایج جستجو برای: mineral chemistry

تعداد نتایج: 173347  

Asahara, , Azizi, , Gholipour, , Masoudi, ,

Zircon is an stable mineral during post crystallization processes and preserves characters of magmatic events. Zircon morphology can give some information about temperature, nature, and source of the magma. Study of the zircon morphology of Cretaceous granitoids and acidic volcanics from the southeast Saqqez area reveals that most of the crystals are P5 and S25 types with high alkalinity (I.A.)...

2005
A. Vlasenko S. Sjogren E. Weingartner K. Stemmler H. W. Gäggeler M. Ammann

Effect of humidity on nitric acid uptake to mineral dust aerosol particles A. Vlasenko, S. Sjogren, E. Weingartner, K. Stemmler, H. W. Gäggeler, and M. Ammann Laboratory of Radioand Environmental chemistry, Paul Scherrer Institute, Villigen, Switzerland Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland Department of Chemistry and Biochemistry, University of Ber...

2014
S. Aravindan

In order to determine mineralogy of rock and soil samples, reflectance and emittance spectroscopy in the near-infra red and short-wave infra-red is used extensively and found to be inexpensive. Hyper spectral remote sensing satellite data are found to be prospective to deliver in depth physico-chemistry like mineralogy, chemistry, morphology of the earth’s surface. Therefore hyper spectral data...

Journal: :British journal of industrial medicine 1993
H Daniel A Wastiaux P Sébastien R Bégin

As well as fibre size, fibre chemistry is a determinant of toxicity of mineral fibres. On these grounds, a few years ago, the asbestos industry in Québec developed a process to modify the surface chemistry of chrysotile asbestos by fixing phosphorous atoms. The pleuropulmonary fibrogenicity and carcinogenicity of the native and surface treated chrysotile, called chrysophosphate, were tested. Bo...

Journal: : 2022

Application of mineral chemistry to mineralization and alteration evaluation in Zn-Pb Angouran deposit, Zanjan

الیاسی, زهرا, امامی, سید نعیم, نصر اصفهانی, علی خان, وهابی مقدم, بابک,

Subplutonic rocks of North Shahrekord at south-west of Iran as a part of Sanandaj - Sirjan tectonical zone have exposed as basic dykes. These rocks are dolerites with specific textures such as intergranular, intersertal, ophitic and poikilitic. The main constituteud minerals of the dolerites are plagioclase and clinopyroxene. The secondary minerals include sericite, calcite, chlorite, epidote, ...

تقی پور, صدیقه, مکی زاده, محمد علی, ترابی, قدرت , تقی‌پور, بتول , خلیلی, محمود, نقره‌ئیان, موسی ,

Several igneous-evaporitic rocks complexes, belonging to Lower Cambrian, are exposed in High Zagros. These rocks exposed parallel to the Zagros main thrust as diapir-shaped bodies. Basaltic rocks are the most common rocks but microgabbro, microdiorite, andesite and trachyte are the rocks of this complex. The studied clinopyroxenes are usually fresh mafic mineral in these rocks and display secto...

2005
YAOTANG WU

Our group has devoted to the application of Nuclear Magnetic Resonance (NMR) spectroscopy and Nuclear Magnetic Resonance Imaging (MRI) to basic science and clinical problems of bone mineral and matrix, and to the diseases associated with bone. NMR spectroscopy provides an analysis of the ionic composition and structure of the mineral crystals and matrix, i.e., the properties of bone as a materi...

2002
Paul R. Bartholomew

This paper is an initial report on the mineral chemistry of four metamorphosed stratabound mineral deposits which are located within or adjacent to the Shuswap Complex. These are commonly referred t” as Cottonbelt, CK, Goldstream and Big I.edge deposits. Rock specimens were selected from those collected by Trygve H6y of the British Columbia Geological Survey Branch. The particular specimens cho...

Ahangari, , Asadpour, , Pashapour, ,

Amphibolites crop out in the NW Salmas as two relatively small bodies around Abati and Ureban villages. Based on petrography and mineral paragenesis, the composition of Abati and Ureban amphibolites consists mainly of epidote amphibolite and amphibolite, respectively. Relict of clinopyroxenes from a parental rock are present in some samples. Mineral paragenesis (high hornblende and plagioclase ...

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