Abstract
An important advance in the FTIR technique in the past decade has been the advent of spectroscopic imaging, which allows a map of the volatile species of interest to be constructed from 4096 simultaneously collected spectra, each of which has a sensitivity approaching larger analyses using conventional FTIR techniques. Here, we introduce the technique and apply it to the analysis of volcanic glasses and melt inclusions from the Izu-Bonin arc to test models for silicic crustal growth, such as differentiation of basaltic material or from melting of pre-existing andesitic lower crust.