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European Journal of Scientific Research (ISSN: 1450 ... - EuroJournals

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© <strong>European</strong> <strong>Journal</strong> <strong>of</strong> <strong>Scientific</strong> <strong>Research</strong>, Vol 7, No 5, 2005<br />

PIXE MICROANALYSIS OF MUSCOVITE SAMPLES FROM TOURMALINE<br />

BEARING GRANITE PEGMATITES OF SOUTHWESTERN NIGERIA<br />

O. A. Ige a , S.O.Olabanji b , D. Ceccatob c<br />

a<br />

Natural History Museum, Obafemi Awolowo University, Ile-Ife, Nigeria<br />

b<br />

National Institute for Nuclear Physics (INFN), National Laboratories <strong>of</strong> Legnaro (LNL), Viale<br />

dell’Università 2, 35020 Legnaro Padua, Italy.<br />

c<br />

ICTP – TRIL fellow on sabbatical leave from Centre for Energy <strong>Research</strong> and Development<br />

(CERD), Obafemi Awolowo University, Ile-Ife, Nigeria.<br />

ABSTRACT<br />

Nearly pure muscovite samples from pegmatite bodies within two different geological<br />

environments have been characterised using an accelerator-based analytical technique <strong>of</strong> PIXE<br />

and Electronprobe microanalyser, in order to determine their major, minor and trace elements<br />

composition and possible industrial application. 17 elements were measured and result shows that<br />

the muscovites from the two localities are generally similar in composition with extensive<br />

substitution in the K and Al sites. Trace element differences such as Au are interpreted as<br />

reflecting the geological environments.<br />

Key words: Muscovites, PIXE, microprobe,trace element.<br />

INTRODUCTION<br />

The analysis <strong>of</strong> trace elements in industrial minerals holds the key to understanding ore metal<br />

pathways and ore formation processes. Proton-induced X-ray emission (PIXE) analysis and the<br />

Electron microprobe provide direct non-destructive methods for the determination <strong>of</strong> the<br />

composition <strong>of</strong> these trace elements with detection limits down to 20 ppm. Muscovite<br />

(Al1.788KMg.64O12Si3.572), <strong>of</strong>ten called white mica, is a rock-forming mineral that has a<br />

layered structure <strong>of</strong> sheets <strong>of</strong> aluminum silicate weakly bonded together by layers <strong>of</strong> potassium<br />

ions. Due to its perfect cleavage, elasticity, and low thermal conductivity, muscovite is <strong>of</strong>ten used<br />

for electrical and thermal insulation applications and also as a lubricant. Finely ground muscovite<br />

is sometimes used to make special surfaces in prints and paintings. It was also used in this<br />

fashion as furnace doors, but its use in this capacity is not as common today because <strong>of</strong> modern<br />

technology alternatives.<br />

Muscovite is a common mineral found all over the world, however most locations do not produce<br />

a high yield product. The largest and most important deposits <strong>of</strong> muscovite are found in the CIS,<br />

Pakistan, India, and Brazil. The United States produces only a small amount <strong>of</strong> high yield sheet<br />

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