Bottom Simulating Reflectors Along the Scan Basin, a Deep-Sea Gateway Between the Weddell Sea (Antarctica) and Scotia Sea
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Publisher
Springer International Publishing
Link
https://link.springer.com/content/pdf/10.1007/978-3-030-81186-0_41
Reference27 articles.
1. Barker PF, Thomas E (2004) Origin, signature and palaeoclimatic influence of the Antarctic Circumpolar Current. Earth Sci Rev 66(1–2):143–162
2. Berndt C, Bünz S, Clayton T et al (2004) Seismic character of bottom simulating reflectors: examples from the mid-Norwegian margin. Mar Pet Geol 21(6):723–733
3. Eagles G, Livermore RA, Fairhead JD et al (2005) Tectonic evolution of the west Scotia Sea. J Geophys Res Solid Earth 110(B2)
4. Emery KO (1974) Pagoda structures in marine sediments. Natural gases in marine sediments. Springer, Boston MA, pp 309–317
5. Galindo-Zaldívar J, Puga E, Bohoyo F et al (2014) Reprint of “Magmatism, structure and age of Dove Basin (Antarctica): a key to understanding South Scotia Arc development.” Glob Planet Change 123:249–268
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