The Wilkes subglacial basin eastern margin electrical conductivity anomaly

We have analyzed the deep conductivity structure at the transition between the Transantarctic Mountains (TAM) and the eastern margin of the WSB in NVL, by means of the GDS (Geomagnetic Deep Sounding) technique, in order to constrain the geodynamical interpretation of this antarctic sector. The TAM f...

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Bibliographic Details
Main Authors: RIZZELLO, DANIELE, ARMADILLO, EGIDIO, Ferraccioli, Fausto, Caneva, Giorgio
Other Authors: Rizzello, Daniele, Armadillo, Egidio
Format: Conference Object
Language:English
Published: 2014
Subjects:
Online Access:http://hdl.handle.net/11567/856358