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- W2084864282 abstract "Abstract The Saxonian Granulite Massif forms a dome structure with a core of high-pressure granulites and minor cordierite-garnet gneisses, and a tectonic cover of lower-grade upper-crustal rocks. Immediately above this tectonic contact, a metamorphic aureole with low-pressure, high-temperature assemblages is developed. Petrological data and structural observations in conjunction with radiometric ages reveal a close link between the near-isothermal decompression path of the granulites, the prograde heating path of their hanging-wall rocks, granitic intrusions, and shear-zone foliations and lineations on both sides of the tectonic contact. To accommodate these features, we propose a “hot core complex” model of asymmetric crustal extension with rapid exhumation of granulitic lower crust along a low-angle detachment zone. As a consequence of high-temperature emplacement of the granulites at shallow-crustal levels, a metamorphic aureole developed in the lower-grade rocks above the shear zone. The extensional unroofing of the granulite complex occurred during the Lower Carboniferous, following the collision stage of the Variscan orogeny." @default.
- W2084864282 created "2016-06-24" @default.
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- W2084864282 date "1994-11-01" @default.
- W2084864282 modified "2023-10-03" @default.
- W2084864282 title "Extensional unroofing of granulitic lower crust and related low-pressure, high-temperature metamorphism in the Saxonian Granulite Massif, Germany" @default.
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- W2084864282 doi "https://doi.org/10.1016/0040-1951(94)90050-7" @default.
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