@article{Tokarski_Antoni_K._Structural_1989,
 author={Tokarski, Antoni K.},
 howpublished={online},
 year={1989},
 abstract={<p>
 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 &#8212; set I, 
 (2) dyking, (3) faulting and, (4) jointing &#8212; set II. Both, folding and 
 subsequent brittle deformation, are hardly compatible with the 
 Mesozoic-Cenozoic eastward subduction of the ancient Pacific ocean crust.
 </p>},
 title={Structural development of Legoupil Formation at Cape Legoupil, Antarctic Peninsula},
 type={Article},
 volume={vol. 10},
 number={No 4},
 journal={Polish Polar Research},
 pages={587-603},
 publisher={Polish Academy of Sciences},
 publisher={Committee on Polar Research},
 keywords={Antarctica, Legoupil Formation, structural geology},
}