Abstract

Fifteen beach sand samples were collected from a depth of 1mt at different locations of the Astaranga beach, Puri with an interval of 300 mts. The beach sand samples were studied for heavy mineral concentration at different location points and were subjected to scanning electron microscope studies for the mineral ilmenite. The percentage of total heavy mineral in Astaranga beach varies from 16.42% to 24.47%. The important minerals are ilmenite, rutile, zircon, sillimanite, garnet, monazite, pyroxene and others. For all samples a set of sieves bearing ASTM nos. 30, 40, 60, 80, 100, 120, 140, 170 and 200 corresponding to 0.59 mm, 0.42 mm, 0.25 mm, 0.177 mm, 0.149 mm, 0.125 mm, 0.105 mm, 0.088 mm and 0.074 mm respectively were used to separate different size fractions. The sieve mesh sizes vary from 0.59 mm to 0.74 mm. It was observed that maximum concentration of heavies was confined to +200 ASTM sieve or 0.74 mm. The total average heavy mineral concentration and light mineral concentration was found to be 20.07% and 79.49% respectively. The concentration percentage of different heavy minerals varied from higher to lower in the order like ilmenite, zircon, sillimanite, garnet, rutile, pyroxene, monazite and others. The ilmenite mineral in this area is found to have altered to secondary phases like pseudorutile, leucoxene and rutile along the fractures, cavities and grain boundaries. The alteration condition was observed as streaks, irregular patches, bands, and rim like structures around the ilmenite grains. Detailed study of alteration in ilmenite was carried out by Energy Dispersive Spectrometer (EDS) attached to Scanning Electron Microscope. The potentialities of heavies found at different locations of the Astaranga beach suggested a good source for the exploration. The alteration of the mineral ilmenite and high concentration of heavy minerals clearly pointed to the sedimentary environment and mechanical concentration process due to repeated wave action.

Highlights

  • The State Odisha (India) is endowed with a long stretch of coast line for a length of 480 km and most part of the coast line is potentially rich with heavy minerals

  • The total heavy minerals percentage has been calculated for different samples collected at different locations

  • The results show the predominance of ilmenite. 3.2

Read more

Summary

Introduction

The State Odisha (India) is endowed with a long stretch of coast line for a length of 480 km and most part of the coast line is potentially rich with heavy minerals. Geochemical characteristics of ilmenite sands of Chhatrapur beach placer deposits of Odisha, India was studied by PIXE and ERXRF methods by Mohanty et al (2003) [6]. They found TiO2 within a range of 52.2 to 56.85 wt %. Rao and Sengupta (2014) [7] studied the ilmenite in the beach placers of Chhatrapur beach, Odisha for texture, micromorphology and elemental composition by XRD and Electronmicrope. They found that the ilmenites have been weathered by chemical and mechanical processes. Surekha Rao and Mishra (2009) studied the sources of ilmenite, monazite, magnetite, etc. by Isodynamic Separator and XRD [8]

Objectives
Methods
Results
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call