The RV Polarstern expedition ANTARKTIS-XXIII/4 (ANT-XXIII/4) began on 10 February 2006 from Punta Arenas returning on 11 April 2006. The main goal of the expedition was to study glaciomarine sedimentation and the evolution of the tectonic-geodynamic setting of the southern Amundsen Sea and Pine Island bay. Crustal and sedimentary structures on the West Antarctic continental margin and Pine Island were surveyed using deep crustal refraction and reflection seismic geophysical methods.
Karsten Gohl, Polina Lemenkova, Jan Grobys, Nicole Parsiegla, Gesa Luise Netzeband, Philipp Schlüter, et al. (2007). Deep crustal refraction and reflection seismics; crustal and sedimentary structures and geodynamic evolution of the West Antarctic continental margin and Pine Island [10.13140/rg.2.2.32124.26240].
Deep crustal refraction and reflection seismics; crustal and sedimentary structures and geodynamic evolution of the West Antarctic continental margin and Pine Island
Polina Lemenkova
Secondo
;
2007
Abstract
The RV Polarstern expedition ANTARKTIS-XXIII/4 (ANT-XXIII/4) began on 10 February 2006 from Punta Arenas returning on 11 April 2006. The main goal of the expedition was to study glaciomarine sedimentation and the evolution of the tectonic-geodynamic setting of the southern Amundsen Sea and Pine Island bay. Crustal and sedimentary structures on the West Antarctic continental margin and Pine Island were surveyed using deep crustal refraction and reflection seismic geophysical methods.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
