NDLI: The Application of Micro-raman Spectroscopy to Distinguish Carlosturanite from Serpentine-group Minerals

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The Application of Micro-raman Spectroscopy to Distinguish Carlosturanite from Serpentine-group Minerals

Content Provider	Semantic Scholar
Author	Elena Belluso Caterina Rinaudo
Copyright Year	2008
Abstract	Carlosturanite, a mineral with a serpentine-like structure, grows mainly with a Þ brous habit. We have analyzed samples with both pure carlosturanite and associations of carlosturanite and chrysotile using micro-Raman spectroscopy, a quick and non-destructive method of identifying different materials and mineral phases through direct analysis of bundles of Þ bers. Raman analysis was carried out on samples after Þ rst submitting them to chemical and mineralogical analysis using traditional techniques, i.e., scanning electron microscopy (SEM) and transmission electron microscopy (TEM), with results evaluated in light of energy-dispersive spectrometry (EDS) and X-ray powder diffractometry (XRPD). This approach allowed us to determine the Raman spectrum associated with carlosturanite. Micro-Raman spectroscopy makes it possible to identify the different phases in these associations of minerals.
File Format	PDF HTM / HTML
Alternate Webpage(s)	http://rruff.info/uploads/CM45_1495.pdf
Language	English
Access Restriction	Open
Subject Keyword	Asbestos, Serpentine Chrysotile Dispersive partial differential equation Ehlers-Danlos Syndrome Extended Data Services Mental association Minerals Raman scattering Scanning Electron Microscopy Spectrometry Spectrometry, X-Ray Emission Spectroscopy, Near-Infrared Transmission Electron Microscopy X-Ray Emission Spectroscopy Ziziphus mauritiana
Content Type	Text
Resource Type	Article

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