Published September 1975
| public
Journal Article
Spectra of shock-affected rhodonite: A reply
Chicago
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Abstract
The Gaussian resolution procedure of Faye (1975) leading to the conclusion that the spectral changes in a shock-loaded rhodonite are the result of a broadening or intensification of the ultraviolet charge-transfer absorption and that the 540 nm band is present with comparable intensity in both pre- and post-shock samples is not physically meaningful because it has ignored the dominant process which gives rise to the rising baseline "absorption" throughout the near-infrared and visible spectral regions. That process is wavelength-dependent scattering.
Additional Information
© 1975 Mineralogical Society of America. Manuscript received, May 1, 1975; accepted for publication, June 5, 1975. Contribution No. 2609: Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California.Additional details
- Eprint ID
- 38173
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- CaltechAUTHORS:20130430-081835615
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2013-05-01Created from EPrint's datestamp field
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2019-11-26Created from EPrint's last_modified field
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- Division of Geological and Planetary Sciences (GPS)
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- Caltech Division of Geological and Planetary Sciences
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- 2609