Combined use of the GGSFT data base and on board marine collected data to model the Moho beneath the Powell Basin, Antarctica

• Main Authors: Chávez Segura, René, Flores Márquez, Elsa Leticia, Suriñach Cornet, Emma, Galindo Zaldívar, Jesús, Rodríguez Fernández, José, Maldonado, Andrés
• Format: Article in Journal/Newspaper
• Language: English
• Published: Universidad de Barcelona; Instituto de Ciencias de la Tierra Jaume Almera 2007
• Subjects: Gravity; Inverse theory; Antartic Peninsula; Powell Basin; Marine geophysics; Antarctic; Antarctic Peninsula; South Scotia Ridge; The Antarctic; Antarc*; Antarctica; antartic*
• Online Access: http://hdl.handle.net/10481/32075

The Powell Basin is a small oceanic basin located at the NE end of the Antarctic Peninsula developed during the Early Miocene and mostly surrounded by the continental crusts of the South Orkney Microcontinent, South Scotia Ridge and Antarctic Peninsula margins. Gravity data from the SCAN 97 cruise o...