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The Mazury complex of northeastern Poland forms a 200 km long, E-W trending anorthosite-mangerite-charnockite-granite belt derived from bimodal, multiphase anorogenic magmatism and is similar to the classic anorogenic complexes of the Fennoscandian Shield (e.g. Wiborg, Salmi and Ragunda). The complex is dominated by felsic and intermediate rocks ranging from quartz monzonite through granodiorite and...
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