نتایج جستجو برای: mineral elements

تعداد نتایج: 339462  

2014
D. D. Cohen A. Paytan M. D. Patey E. P. Achterberg J P. Engelbrecht K. W. Fomba

Introduction Conclusions References Tables Figures

2015
M Angeline Christie Hannah S Krishnakumari

Dietary elements, commonly known as dietary minerals are chemical elements required by living organisms other than the elements present in the common organic molecules. Dietary fibre and minerals are important for healthy functioning of the human body. The mineral nutrition is an important aspect and its pivotal role in human life provides healthy growth. The present study was undertaken to ana...

Journal: :The American mineralogist 2014
Zhen Li Jill D Pasteris

Carbonate-substituted hydroxylapatite is the inorganic component in bone. The nanometer size of bone crystallites and their interweaving with subequal volumes of collagen fibrils make the chemical analysis of the bone mineral extremely difficult. The few chemical analyses that are available commonly were made on ashed bone, which, in addition to mineral, also includes chemical residues of colla...

2014
Lu Zhao Zhidan Xia Fudi Wang

Iron, copper, zinc, and eight other minerals are classified as essential trace elements because they present in minute in vivo quantities and are essential for life. Because either excess or insufficient levels of trace elements can be detrimental to life (causing human diseases such as iron-deficiency anemia, hemochromatosis, Menkes syndrome and Wilson's disease), the endogenous levels of trac...

Journal: :Spectrochimica acta. Part A, Molecular and biomolecular spectroscopy 2015
Ray L Frost Andrés López Frederick L Theiss Ricardo Scholz Antônio Wilson Romano

We have studied the mineral normandite using a combination of scanning electron microscopy with energy dispersive spectroscopy and vibrational spectroscopy. The mineral normandite NaCa(Mn(2+),Fe(2+))(Ti,Nb,Zr)Si2O7(O,F)2 is a crystalline sodium calcium silicate which contains rare earth elements. Chemical analysis shows the mineral contains a range of elements including Na, Mn(2+), Ca, Fe(2+) a...

2017
Elizabeth J. Catlos Nathan R. Miller

Monazite [(Ce,Th)PO4] from the Llallagua tin ore deposit in Bolivia is characterized by low radiogenic element contents. Previously reported field evidence and mineral associations suggest the mineral formed via direct precipitation from hydrothermal fluids. Monazite compositions thus may provide insight into characteristics of the fluids from which it formed. Chemical compositions of three Lla...

2013
D. Zannoni A. Quaranta G. Valotto G. Rampazzo

Scheelite is a calcium tungstate mineral (CaWO4) well known in the mining industry as a source of tungsten. This mineral fluoresces under shortwave UV and X-rays excitation with a characteristic blue luminescence centered at about 425 nm. CaWO4-based powder was commonly used as blue phosphor and scintillator (due to high Z of W) [1-3]. The emitted spectrum shifts to yellow in the presence of mo...

Journal: :iranian journal of earth science 0
jamal tarrah islamic azad university, bandar abbas branch, geology department, bandar abbas, iran zahra abedpour islamic azad university, bandar abbas branch, geology department, bandar abbas, iran karl strauss institute of mineralogy-geochemistry and salt deposits, university of clausthal, germany thomas schirmer institute of mineralogy-geochemistry and salt deposits, university of clausthal, germany kurt mengel institute of mineralogy-geochemistry and salt deposits, university of clausthal, germany

ten chromite ores from ophiolite complexes in se iran were analyzed mineralogically by xrd, chemically by xrf, and mineral chemistry by epma. the identified paragenesis of silicate minerals of chromite ores with the x-ray diffraction is pronounced differently. it consists of secondary phases formed as serpentine, cr-containing chlorite (kaemmererite), chromic garnet (uarovite) with preserved pa...

Jamal Tarrah, Karl Strauss Kurt Mengel Thomas Schirmer Zahra Abedpour

Ten chromite ores from ophiolite complexes in SE Iran were analyzed mineralogically by XRD, chemically by XRF, and mineral chemistry by EPMA. The identified paragenesis of silicate minerals of chromite ores with the X-ray diffraction is pronounced differently. It consists of secondary phases formed as serpentine, Cr-containing chlorite (kaemmererite), chromic garnet (uarovite) with preserved pa...

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