Tectonic development of the Bransfield Basin and its prolongation to the South Scotia Ridge, northern Antarctic Peninsula

Author:

Galindo-Zaldı́var Jesús,Gamboa Luiz,Maldonado Andrés,Nakao Seizo,Bochu Yao

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference52 articles.

1. Transtensional tectonics along the South Scotia Ridge, Antarctica;Acosta;Tectonophysics,1996

2. Acosta, J., Canals, M., Alonso, B., ORCA Group, 1994. Bathymetry of the Hesperides Deep, Scotia Sea, South Scotia Ridge, Antarctica. Map scale 1:200.000, University of Barcelona, Barcelona.

3. Tectonics of the triple junction at the southern end of the Shackleton Fracture Zone (Antarctic Peninsula);Aldaya;Geo Mar. Lett.,1996

4. Crustal structure of the South Shetland Islands and Bransfield Strait;Ascroft;Sci. Rep. Br. Antarct. Surv.,1972

5. The Cenozoic subduction history of the Pacific margin of the Antarctic Peninsula: ridge crest–trench interactions;Barker;J. Geol. Soc. (Lond.),1982

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