Magmatic evolution and tectonic setting of metabasites from Lützow-Holm Complex, East Antarctica
Metabasites from the Lützow-Holm Complex, East Antarctica, are the equivalent of metamorphosed ultramafic and mafic rocks with ultrabasic to intermediate compositions, which occur as layers and blocks in the quartzo-feldspathic or metasedimentary gneisse
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|Source:||Geological Society of London Special Publication|
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