Summary 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 lakes
The Antarctic geomagnetics community remains very active in crustal anomaly mapping. Several interna...
Summary The most recent subglacial lake inventories and classification methods further demonstrate t...
The Wilkes Subglacial Basin (WSB) represents a largely unexplored, approximately 1400 km-long and up...
As we enter the IPY geological boundary conditions for the stability of the East Antarctic Ice Sheet...
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...
Airborne geophysical surveys play a pivotal role in imaging subglacial geology and characterizing br...
A high-resolution (1 km line spacing) aerogeophysical survey was conducted over a region near the Ea...
In the 2016-2017 austral summer, the University of Texas Institute for Geophysics (UTIG) and the Kor...
The Wilkes Subglacial Basin (WSB) extends for 1,400 km from George V Land into the interior of East ...
Subglacial hydrology in East Antarctica is poorly understood, yet may be critical to the manner in w...
The Wilkes Subglacial Basin (WSB) extends for ca 1,400 km into the interior of East Antarctica and ...
The Antarctic geomagnetics' community remains very active in crustal anomaly mapping. More than 1.5 ...
The Ross Ice Shelf controls the flow of ice into the ocean from catchments consisting of both the Ea...
The Antarctic geomagnetics community remains very active in crustal anomaly mapping. Several interna...
Summary The most recent subglacial lake inventories and classification methods further demonstrate t...
The Wilkes Subglacial Basin (WSB) represents a largely unexplored, approximately 1400 km-long and up...
As we enter the IPY geological boundary conditions for the stability of the East Antarctic Ice Sheet...
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...
Airborne geophysical surveys play a pivotal role in imaging subglacial geology and characterizing br...
A high-resolution (1 km line spacing) aerogeophysical survey was conducted over a region near the Ea...
In the 2016-2017 austral summer, the University of Texas Institute for Geophysics (UTIG) and the Kor...
The Wilkes Subglacial Basin (WSB) extends for 1,400 km from George V Land into the interior of East ...
Subglacial hydrology in East Antarctica is poorly understood, yet may be critical to the manner in w...
The Wilkes Subglacial Basin (WSB) extends for ca 1,400 km into the interior of East Antarctica and ...
The Antarctic geomagnetics' community remains very active in crustal anomaly mapping. More than 1.5 ...
The Ross Ice Shelf controls the flow of ice into the ocean from catchments consisting of both the Ea...
The Antarctic geomagnetics community remains very active in crustal anomaly mapping. Several interna...
Summary The most recent subglacial lake inventories and classification methods further demonstrate t...
The Wilkes Subglacial Basin (WSB) represents a largely unexplored, approximately 1400 km-long and up...