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NASA NTRS · 20040059921

Synchrotron X-Ray Diffraction Analysis of Meteorites in Thin Section: Preliminary Results

Abstract

X-ray diffraction is the pre-eminent technique for mineral identification and structure determination, but is difficult to apply to grains in thin section, the standard meteorite preparation. Bright focused X-ray beams from synchrotrons have been used extensively in mineralogy and have been applied to extraterrestrial particles. The intensity and small spot size achievable in synchrotron X-ray beams makes them useful for study of materials in thin sections. Here, we describe Synchrotron X-ray Diffraction (SXRD) in thin section as done at the National Synchrotron Light Source, and cite examples of its value for studies of meteorites in thin section.

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Treiman, A. H., Lanzirotti, A., Xirouchakis, D.. 2004-01-01. Synchrotron X-Ray Diffraction Analysis of Meteorites in Thin Section: Preliminary Results. https://ntrs.nasa.gov/citations/20040059921

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