As we enter the IPY geological boundary conditions for the stability of the East Antarctic Ice Sheet (EAIS) remain largely unknown. During the 2005/06 field season a major new aerogeophysical survey was performed over the Wilkes Subglacial Basin, the Transantarctic Mountains and Dome C. Over 60,000 km of new airborne radar, aeromagnetic and aerogravity data were collected. We will describe the survey layout and methodologies and present new geophysical images as a tool to address the highly contentious stability of the EAIS during warmer than present palaeoclimates, the underlying crustal structure, and to study subglacial lake
The region around Dome Fuji is considered as one of the most suitable areas in East Antarctica to fi...
The Wilkes Subglacial Basin extends for ca 1,400 km from George V Land into the interior of East Ant...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...
Summary As we enter the IPY geological boundary conditions for the stability of the East Antarctic I...
An extensive aerogeophysical survey was flown in Wilkes Land (East Antarctica) during the 2005/06 An...
The Wilkes Subglacial Basin (WSB) extends for ca 1,400 km from George V Land into the interior of Ea...
The Wilkes Subglacial Basin represents an approximately 1400 km-long and up to 600 km wide subglacia...
Topography, sediment distribution, and heat flux are all key boundary conditions governing the dynam...
A high-resolution (1 km line spacing) aerogeophysical survey was conducted over a region near the Ea...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...
Airborne geophysical surveys play a pivotal role in imaging subglacial geology and characterizing br...
The Wilkes Subglacial Basin (WSB) extends for ca 1,400 km into the interior of East Antarctica and ...
The Wilkes Subglacial Basin extends for 1,400 km into the interior of East Antarctica and hosts seve...
"A thesis submitted for the degree of Doctor of Philosophy""November, 2011"No signed consent form fo...
The region around Dome Fuji is considered as one of the most suitable areas in East Antarctica to fi...
The Wilkes Subglacial Basin extends for ca 1,400 km from George V Land into the interior of East Ant...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...
Summary As we enter the IPY geological boundary conditions for the stability of the East Antarctic I...
An extensive aerogeophysical survey was flown in Wilkes Land (East Antarctica) during the 2005/06 An...
The Wilkes Subglacial Basin (WSB) extends for ca 1,400 km from George V Land into the interior of Ea...
The Wilkes Subglacial Basin represents an approximately 1400 km-long and up to 600 km wide subglacia...
Topography, sediment distribution, and heat flux are all key boundary conditions governing the dynam...
A high-resolution (1 km line spacing) aerogeophysical survey was conducted over a region near the Ea...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...
Airborne geophysical surveys play a pivotal role in imaging subglacial geology and characterizing br...
The Wilkes Subglacial Basin (WSB) extends for ca 1,400 km into the interior of East Antarctica and ...
The Wilkes Subglacial Basin extends for 1,400 km into the interior of East Antarctica and hosts seve...
"A thesis submitted for the degree of Doctor of Philosophy""November, 2011"No signed consent form fo...
The region around Dome Fuji is considered as one of the most suitable areas in East Antarctica to fi...
The Wilkes Subglacial Basin extends for ca 1,400 km from George V Land into the interior of East Ant...
The East Antarctic Ice Sheet (EAIS) is underlain by a series of low‐lying subglacial sedimentary bas...