The hydrous components in garnets; grossular-hydrogrossular

Abstract

Grossular garnets from 33 localities were examined for indications of OH- or H_2O in their infrared spectrum. All contained OH-. Classical hydrogrossular with more than 5
\nwt% H_2O displays systematics pectroscopic behavior consistent with the hydrogarnet substitution consisting of two absorption bands at 3598 and 3662 cm^(-1). These spectroscopic characteristics were generally not observed in other glossular samples. Instead, 20 distinct
\nabsorption bands have been identified in the spectra of common grossular, occurring in groups of four to ten bands. Both the number and intensities of these bands show a large
\nvariation, which does not correspond with the garnet's composition. Seven classes of spectra were identified in the OH region based on the position of the most intense absorption band. The spectroscopic data suggest that in addition to the tetrahedral site, OH groups exist in multiple other environments. The OH content of grossular garnets can be obtained from infrared spectra using the equation H_2O wt% = 0.0000786 x integrated absorbance per cm in the OH region near 3600 cm^(-1). The OH content of macroscopic grossular crystals (expressed as weight percent H_2O) ranged from 12.8% doown to less than 0.005%. Macroscopic grossular typically contains less than 0.3 wt% H_2O. Grossular from rodingites and low-temperature alteration vugs contained much more than that from
\nskarn or contact metamorphic environments.