TY - JOUR N2 - Rocks of the Legoupil Formation in the Cape Legoupil area were folded about a N70E oriented axis. Later these rocks were affected only by brittle deformation which occurred in four stages: (1) jointing — set I, (2) dyking, (3) faulting and, (4) jointing — set II. Both, folding and subsequent brittle deformation, are hardly compatible with the Mesozoic-Cenozoic eastward subduction of the ancient Pacific ocean crust. L1 - http://www.journals.pan.pl/Content/111246/PDF-MASTER/1989_4_587-603.pdf L2 - http://www.journals.pan.pl/Content/111246 PY - 1989 IS - No 4 EP - 603 KW - Antarctica KW - Legoupil Formation KW - structural geology A1 - Tokarski, Antoni K. PB - Polish Academy of Sciences PB - Committee on Polar Research VL - vol. 10 DA - 1989 T1 - Structural development of Legoupil Formation at Cape Legoupil, Antarctic Peninsula SP - 587 UR - http://www.journals.pan.pl/dlibra/publication/edition/111246 T2 - Polish Polar Research ER -