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- W2003135149 abstract "In the Koralpe and Saualpe polycrystalline basement, which is now a part of the Austroalpine nappe system, eclogites and metagabbros occur intercalated in gneisses and kyanite-bearing schists. We report here the chemical as well as Sr- and O-isotopic composition of such eclogites and one metagabbro. A low-Ti kyanite-bearing and a high-Ti kyanite-free group can be distinguished which may be related by igneous differentiation. The low-Ti group which comprises eclogites and the metagabbro has chemical characteristics indicating formation of the igneous precursors as cumulates by crystallization of pyroxene and plagioclase from a mafic magma. In contrast, the protoliths of the high-Ti eclogites appear to be basaltic liquids with normal- to enriched-type MORB affinities which are likely to have formed at an oceanic ridge. Their Sr- and O-isotope relationships strongly suggest that they have suffered both a phase of low temperature and a phase of high-temperature hydrothermal alteration by reaction with seawater." @default.
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- W2003135149 date "1988-01-01" @default.
- W2003135149 modified "2023-10-02" @default.
- W2003135149 title "Geochemistry and origin of eclogites from the type locality Koralpe and Saualpe, Eastern Alps, Austria" @default.
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- W2003135149 doi "https://doi.org/10.1016/0009-2541(88)90009-5" @default.
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