Recent morpho-sedimentary processes in Dove Basin, southern Scotia Sea, Antarctica: A basin-scale case of interaction between bottom currents and mass movements

Author:

Lobo F.J.,López-Quirós A.,Hernández-Molina F.J.,Pérez L.F.,García M.,Evangelinos D.,Bohoyo F.,Rodríguez-Fernández J.,Salabarnada A.,Maldonado A.

Funder

Gobierno de España Ministerio de Ciencia e Innovación

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference83 articles.

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3. Scotia Sea regional tectonic evolution: implications for mantle flow and palaeocirculation;Barker;Earth-Science Rev.,2001

4. Heat-flow determinations of basement age in small oceanic basins of the southern central Scotia Sea;Barker;Geol. Soc. London Spec. Publ.,2013

5. Extensional deformation and development of deep basins associated with the sinistral transcurrent fault zone of the Scotia Antarctic plate boundary;Bohoyo,2007

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