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Original Articles

HIGH DENSITY MINERAL INCLUSIONS IN ROCKS EVIDENCED BY γ-RAY TOMODENSITOMETRY

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Pages 119-129 | Received 23 Feb 2000, Accepted 03 Jul 2000, Published online: 16 Feb 2007
 

Abstract

A fragment of a polysulfide rock containing quartz and high density mineral inclusions has been investigated by using a 192Ir γ-ray dual computer tomograph. The tomographic image revealed the existence of three different mineral fractions, whose densities and effective atomic numbers, as calculated by means of the image histograms, were equal to 2.57 ± 0.24 × 103 kg/m3 (Z eff = 11.6 ± 2.1), 4.01 ± 0.22 × 103 kg/m3 (Z eff = 25.1 ± 2.1), and 6.01 ± 0.90 × 103 kg/m3 (Z eff = 68.5 ± 6.0), respectively. Subsequently, these minerals were identified as quartz, a complex mixture of medium density polymetallic sulfide (pyrite, blenda, chalcopyrite, and sphalerite), and galena as heavier component. A detailed mineralogical analysis confirmed these data.

ACKNOWLEDGMENTS

We are grateful to Mihai Atanasiu M.S. for his help in describing the mineralogy of the investigated sample.

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