Abstract
Alteration phenomena in hornblende crystals of the northwestern Okchon metamorphic belt were investigated in detail using high-resolution transmission electron microscopy (HRTEM). HRTEM images of hornblende commonly show submicroscopic intergrowths of a variety of sheet silicates; chlorite is the most abundant sheet silicate within hornblende, and biotite is also frequently observed along with chlorite. Although the angle between (001) of chlorite and (100) of hornblende is variable, the (001) planes of both chlorite and biotite parallel the c axis of hornblende. Microstructural evidences indicate that both sheet silicates intergrown with hornblende are produced by retrogression of hornblende. Biotite apparently formed by early hydration reaction in the presence of fluids enriched with K+, and chlorite at a later stage of retrograde reaction when K+ was consumed. In addition, hornblende crystals contain numerous etch pits and poorly crystalline silicates as filling materials, which are the product of weathering. Such submicroscopic intergrowths of sheet silicates may result in somewhat high Al contents in the hornblende analysis, producing imprecise result in geothermobarometric calculations. Furthermore, submicroscopic alteration of hornblende deteriorates the Ar retentivity and consequently affects the K−Ar isotopic ages or the40Ar/39Ar age spectra of hornblende. It is thus evident that the HRTEM characterization of hornblende is prerequisite for the correct interpretation of P-T estimates and age data.
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Ahn, J.H., Cho, M. Submicroscopic alteration of hornblende in the amphibolitic schists, northwestern Okchon metamorphic belt. Geosci J 2, 165–174 (1998). https://doi.org/10.1007/BF02910162
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DOI: https://doi.org/10.1007/BF02910162