@ARTICLE{Tokarski_Antoni_K._Structural_1989,
 author={Tokarski, Antoni K.},
 volume={vol. 10},
 number={No 4},
 journal={Polish Polar Research},
 pages={587-603},
 howpublished={online},
 year={1989},
 publisher={Polish Academy of Sciences},
 publisher={Committee on Polar Research},
 abstract={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.},
 type={Article},
 title={Structural development of Legoupil Formation at Cape Legoupil, Antarctic Peninsula},
 URL={http://journals.pan.pl/Content/111246/PDF-MASTER/1989_4_587-603.pdf},
 keywords={Antarctica, Legoupil Formation, structural geology},
}