Fingerprinting the water site in mantle olivine

By A. Berry, J. Hermann, H. O’Neill, G. Foran. 2005

213 citations recorded by the source corpus.

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

A review of water contents of nominally anhydrous natural minerals in the mantles of Earth, Mars and the Moon (2010, background): “Although Ti may play a role in H incorporation in Ol (Berry et al., 2005), no conclusive correlations between Ti and water contents of Ol have been observed (Matveev and Stachel, 2007).”
Intercalibration of FTIR and SIMS for hydrogen measurements in glasses and nominally anhydrous minerals (2007, background): “…more than 40 infrared absorption bands identiÞ ed so far (e.g., Bai and Kohlstedt 1992, 1993; Bell 1992; Bell et al. 2003; Beran and Putnis 1983; Berry et al. 2005; Freund and Oberheuser 1986; Khisina and Wirth 2002; Kitamura et al. 1987; Kohlstedt et al. 1996; Lemaire et al. 2004; Matsyuk and…”
Mechanisms of hydrogen incorporation and diffusion in iron-bearing olivine (2006, background): “In their study, Berry et al. (2005) attributed the IR bands near 3,572 and 3,525 cm , regularly observed in natural olivine, to the presence of Ti-clinohumite-like defects (TEM investigations have not been reported to confirm the presence of such defects in the samples studied by Berry et al.”