The Sudetic ophiolite: current view on its geodynamic model

Elżbieta Dubińska, Piotr Gunia

Abstract


Newly acquired geochemical data on the geochemistry of rodingites and amphibolites from ultrabasic massifs adjacent to Góry Sowie block combined with other available data in the literature, show that Sudetic ophiolite can be interpreted as “surviving” fragment of obducted rock series previously formed in MOR regime and overthrusted onto Góry Sowie block.


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