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