Evolution of the Pacific margin of the northern Antarctic Peninsula: an overview

@article{Birkenmajer1994EvolutionOT,
  title={Evolution of the Pacific margin of the northern Antarctic Peninsula: an overview},
  author={Krzysztof Birkenmajer},
  journal={Geologische Rundschau},
  year={1994},
  volume={83},
  pages={309-321}
}
The sector of the northern Antarctic Peninsula between the Tula and Shackleton Fracture Zones provides evidence for the subduction of south-east Pacific oceanic crust under Antarctic continental crust during Late Mesozoic through Miocene times. The pre-subduction depositional history of this sector includes the formation of a marine siliciclastic turbidite wedge (?Permian-Triassic) deposited in a marginal basin setting. It was folded and thrust retroarc before the Middle Jurassic to form the… 

Chapter 3.1b Antarctic Peninsula and South Shetland Islands: petrology

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