INVESTIGADORES
VARELA Maria Eugenia
congresos y reuniones científicas
Título:
RAMAN, FTIR, AND MÖSSBAUER SPECTROSCOPY OF
Autor/es:
ABDU, Y.; VARELA M.E.; HAWTHORNE F.
Lugar:
Greenwich
Reunión:
Congreso; 74th Annual Meteoritical Society Meeting (2011); 2011
Institución organizadora:
Meteoritical Soc- NASA
Resumen:
Olivine is a major basaltic mineral in hightemperature volcanic rocks and in stony meteorites. The D?Orbigny angrite contains large olivine crystals (up to ~ 1 cm in size) that are present throughout the rock, mimicking xenocrysts or forming olivinite (polycrystalline olivine) [1-3]. The olivinites are of particular interest, as very little is known about them. Here,we study three types of D?Orbigny olivines: honey olivine (HOl),green olivine (GOl), and olivinite (POl), by Raman, Fourier transform infrared (FTIR), and Mössbauer spectroscopy, and compare their structural and spectral features.
