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...
Main Authors: | , , , |
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Other Authors: | , |
Format: | Conference Object |
Language: | English |
Published: |
2014
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Subjects: | |
Online Access: | http://hdl.handle.net/11567/856358 |