Formation of low‐pressure reaction textures during near‐isothermal exhumation of hot orogenic crust (Bohemian Massif, Austria)

Abstract

AbstractTwo types of aluminous paragneiss from the Loosdorf complex (Bohemian Massif, NE Austria) contain coarse‐grained granulite assemblages and retrograde reaction textures that are investigated to constrain the post‐peak history of the Gföhl unit in the southern Bohemian Massif. Both types have a peak assemblage garnet–biotite–sillimanite–plagioclase–K‐feldspar–quartz–granitic melt ± kyanite ± ilmenite ± rutile, recording peak metamorphic conditions of 0.9–1.1 GPa and 780–820°C estimated by isochemical phase equilibrium modelling. The first sample type (Ysper paragneiss) developed (i) cordierite coronae around garnet and (ii) cordierite–spinel and cordierite–quartz reaction textures at former garnet–sillimanite interfaces. Calculated chemical potential relationships indicate that the textures formed in the course of a post‐peak near‐isothermal decompression path reaching 0.4 GPa. Texture formation follows a two‐step process. Initially, cordierite coronae grow between garnet and sillimanite. As these coronae thicken, they facilitate the development of local compositional domains, leading to the formation of cordierite–spinel and cordierite–quartz symplectites. The second sample type (Pielach paragneiss) exhibits only discontinuous cordierite coronae around garnet porphyroblasts but lacks symplectites. The formation of cordierite there also indicates near‐isothermal decompression to 0.4–0.5 GPa and 750–800°C. This relatively hot decompression path is explained by the contemporaneous exhumation of a large HP–UHT granulite body now underlying the Loosdorf complex. The timing of regional metamorphism in the granulites and the southern Bohemian Massif in general is well constrained and has its peak at 340 Ma. Monazite from Loosdorf paragneiss samples yield a slightly younger age of 335 Ma. Although the ages overlap within error, they are interpreted to reflect near‐isothermal decompression and exhumation resulting in the formation of the observed reaction textures.