Abstract
Two basaltic glass samples have been studied, one from the Masaya volcano in Nicaragua and one from the Villarrica volcano in Chile using 57Fe Mössbauer spectroscopy. The iron(II) to iron(III) ratio has been determined for each sample. The 80 K data shows some separation of the sites and is fitted allowing for discrete doublets.
Similar content being viewed by others
References
Stoiber, R.E., Williams, S.N., Huebert, B.: J. Volcanol. Geotherm. Res. 33, 1 (1987)
Andres, R.J., Kasgnoc, A.D.: J. Geophys. Res. 103, 25251–25261 (1998)
Halmer, M.M., Schmincke, H.-U., Graf, H.F.: J. Volcanol. Geotherm. Res. 115, 511 (2002)
Mather, T.A., Tsanev, V.I., Pyle, D.M., McGonigle, A.J.S., Oppenheimer, C., Allen, A.G.: J. Geophys. Res. 109, D21303 (2004)
McCammon, C.A.: EMU Notes Mineral. 6, 369–398 (2004), Chapter 9
Wilke, M., Partzsch, T.G.M., Bernhardt, R., Lattard, D.: Chem. Geol. 220, 143 (2005)
Mather, T.A., McCabe, J.R., Kumar Rai, V., Thiemens, M.H., Pyle, D.M., Heaton, T.H.E., Sloane, H.J., Fern, G.R.: J. Geophys. Res. 111(D18), D18205 (2006)
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Fern, G.R., Mather, T.A. & Pyle, D.M. Investigation of near-source basaltic glasses using 57Fe Mössbauer spectroscopy. Hyperfine Interact 166, 705–708 (2005). https://doi.org/10.1007/s10751-006-9345-y
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10751-006-9345-y