The Sudetic ophiolite: current view on its geodynamic model

Authors

  • Elżbieta Dubińska Instytut Geochemii, Mineralogii i Petrografii, Uniwersytet Warszawski, 02-089 Warszawa, al. Żwirki i Wigury 93
  • Piotr Gunia Instytut Nauk Geologicznych, Uniwersytet Wrocławski, 50-204 Wrocław, pl. Maxa Borna 9

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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Published

2013-02-21

Issue

Vol. 41 No. 1 (1997)

Section

Articles

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