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Asymmetric boudinage of granitic dykes of the Granite Harbour Igneous Complex intruded in amphibolite-facies metasediments of the Wilson Terrane (Renninck schist) (Mt. Weihaupt, Ross Orogen, Antarctica). PhotoID184

Asymmetric boudinage of granitic dykes of the Granite Harbour Igneous Complex intruded in amphibolite-facies metasediments of the Wilson Terrane (Renninck schist) (Mt. Weihaupt, Ross Orogen, Antarctica). PhotoID184

Photograph: R. Carosi

Reference: Roland N. W., Olesh M., Shubert W. (1989) – Geology and Petrology of the Western border of the Transantarctic Mountains, between the Outback Nunataks and Reeves Glacier, Northern Victoria Land, Antarctica. Geol. Jb., E 38, 119-141.