Characterization and luminescent properties of thermally annealed olivines

Olivine is an iron-magnesium solid solution silicate (Mg,Fe)2SiO4 and it is probably one of the most abundant mineral phase in the Solar System, it is present in the primitive carbonaceous meteorites (i.e Allende), and in ordinary chondritic meteorite, comets or terrestrial planets. The olivine grai...

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Veröffentlicht in:	Radiation measurements 2013-09, Vol.56, p.262-266
Hauptverfasser:	Colin-Garcia, Maria, Correcher, Virgilio, Garcia-Guinea, Javier, Heredia-Barbero, Alejandro, Roman-Lopez, Jesus, Ortega-Gutierrez, Fernando, Negron-Mendoza, Alicia, Ramos-Bernal, Sergio
Format:	Artikel
Sprache:	eng
Schlagworte:	Cathodoluminescence Earth sciences Earth, ocean, space Exact sciences and technology Geochronology Iron Isotope geochemistry. Geochronology Luminescence Magnesium Minerals Olivine Solar system Thermal annealing Thermoluminescence
Online-Zugang:	Volltext
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