ePIC

Vibroseis versus Explosive Reflection Seismics at the local dome Halvfarryggen; Antarctica.

Edit Item Edit Item

General Information:

Citation:
Hofstede, C. , Diez, A. , Eisen, O. , Kristoffersen, Y. and Jansen, D. (2012): Vibroseis versus Explosive Reflection Seismics at the local dome Halvfarryggen; Antarctica. , The Geophysics of the Cryosphere and Glacial Products: Properties, Processes and Technical Advances: New Advances in Geophysics Meeting 2012 British Geophysical Association/Royal Astronomical Society/The Geological Society, London, Burlington House, 9 February 2012 - 10 February 2012 .
Cite this page as:
Contact Email:
Download:

Supplementary Information:

Abstract:

The first Vibroseis reflection survey at Antarctica was successfully carried out by AWI in 2010. Based on the results the vibrator in combination with a snow streamer gave, a grid survey was carried out at Halvfarryggen in 2011. Halvfarryggen is a local 900m thick ice dome close to the grounding line in the vicinity of the German research station Neumayer III. Here we present the results of the Vibroseis reflection survey where we focus on the stratigraphy of the underlying strata of the dome. From the main grid line seismic reflection data were also collected using explosives. Resolution and penetration of the Vibroseis and explosive data sets are compared and discussed as well as the logistics of each method.

Further Details:

Imprint
AWI
Policies:
read more
OAI 2.0:
http://epic.awi.de/cgi/oai2
ePIC is powered by:
EPrints 3