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Research Training Program
VIRTUAL POSTER SESSION
2004


Cathodoluminescence Analysis of Six Bayon Style Sculptures from Angkor Wat, Cambodia

Lee Zelewicz
Research Training Program, 2004



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ABSTRACT

Six samples from Khmer sandstone sculptures dating to the 12th-13th centuries from the collections of the National Museum of Cambodia were studied by cathodoluminescence (CL). Macro- and some microscopic study suggested that these six sculptures from Angkor Wat appear to be carved from the same sandstone. Thin-sections, small samples roughly 1 cm by ½ cm and cut paper thin, were obtained from each sculpture. These thin-sections were observed with CL a technique that images the distribution of trace elements within mineral grains. To use CL, the sample is placed under a vacuum, and an electron beam is directed on the sample. Minerals luminesce in different colors, which makes it possible to differentiate among mineral types. CL images were taken of each sample and compiled into a composite showing the whole sample as imaged with CL. These CL mosaics were modified in Photoshop to create color-maps, showing each mineral subtype in a different color, so they can be identified and categorized to obtain a pixel percentage of each mineral subtype within a sample.


Digital Maps

Digital maps were created using digital imaging equipment, and then they were used as maps for the CL imaging

Cathodoluminescence Maps

Cathodoluminescence Maps are used for mineral identification. Each mineral luminesces in different colors, which makes identification possible.

Mineral Subtypes

Mineral Subtypes were taken with the CL and supplied examples of the minerals that are present in each sample. The subtypes supplied the characteristics that define a mineral group. (K1695 subtypes shown)


CONCLUSIONS

The six samples are similar in composition, and thus most likely have a common geological provenance. Quartz and feldspars, which are the predominant mineral components of these sandstones, showed similar luminescence features and class proportions. Other grains in the sandstones were derived from altered rock sources are in present in similar proportions. The results of this study corroborate other types of petrographic analysis of these samples, and further supporting the hypothesis that the sandstone of these sculptures came from the same geological unit, and perhaps even the same quarry.


ACKNOWLEDGEMENTS

NSF, Department of Mineral Sciences, Lisa Collins, Tim Rose, Mary Sangrey, Freer / Sackler, The National Museum of Cambodia, & NMNH

This research was supported by a grant to the NMNH Research Training Program from the National Science Foundation Research Experiences for Undergraduates program, Award Number DBI-0243512.


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The information presented here represents preliminary research as the result of ten-weeks of investigation in-residence at the National Museum of Natural History. This is not an official publication of the information.

As preliminary information, results and/or findings should not be cited as part of conclusive work. Please contact the authors first if you wish to utilize the information presented here.

 

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