Seismics on Ice
Seismic reflection methods can very well be used in glaciology. How does this method work? What is a CMP gather and how do we convert recorded data into a map of the subsurface? What are important parameters to consider when setting up a survey. I will discuss three field surveys at very different l...
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ftawi:oai:epic.awi.de:25144 2023-05-15T16:41:53+02:00 Seismics on Ice Hofstede, Coen Diez, Anja Eisen, Olaf Kristoffersen, Y. 2011-10-07 https://epic.awi.de/id/eprint/25144/ https://hdl.handle.net/10013/epic.38314 unknown Hofstede, C. orcid:0000-0002-6015-6918 , Diez, A. , Eisen, O. orcid:0000-0002-6380-962X and Kristoffersen, Y. (2011) Seismics on Ice , Antarctic Glaciology workshop, Norsk Polar Institutt, Tromsø . hdl:10013/epic.38314 EPIC3Antarctic Glaciology workshop, Norsk Polar Institutt, Tromsø Conference notRev 2011 ftawi 2021-12-24T15:35:19Z Seismic reflection methods can very well be used in glaciology. How does this method work? What is a CMP gather and how do we convert recorded data into a map of the subsurface? What are important parameters to consider when setting up a survey. I will discuss three field surveys at very different locations in ice: An ice shelf, a local ice dome and a mountain glacier. Each site has its own specific problems and advantages. At all survey sites I will compare two source types: conventional explosives against vibrator data. Conference Object Ice Shelf Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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unknown |
description |
Seismic reflection methods can very well be used in glaciology. How does this method work? What is a CMP gather and how do we convert recorded data into a map of the subsurface? What are important parameters to consider when setting up a survey. I will discuss three field surveys at very different locations in ice: An ice shelf, a local ice dome and a mountain glacier. Each site has its own specific problems and advantages. At all survey sites I will compare two source types: conventional explosives against vibrator data. |
format |
Conference Object |
author |
Hofstede, Coen Diez, Anja Eisen, Olaf Kristoffersen, Y. |
spellingShingle |
Hofstede, Coen Diez, Anja Eisen, Olaf Kristoffersen, Y. Seismics on Ice |
author_facet |
Hofstede, Coen Diez, Anja Eisen, Olaf Kristoffersen, Y. |
author_sort |
Hofstede, Coen |
title |
Seismics on Ice |
title_short |
Seismics on Ice |
title_full |
Seismics on Ice |
title_fullStr |
Seismics on Ice |
title_full_unstemmed |
Seismics on Ice |
title_sort |
seismics on ice |
publishDate |
2011 |
url |
https://epic.awi.de/id/eprint/25144/ https://hdl.handle.net/10013/epic.38314 |
genre |
Ice Shelf |
genre_facet |
Ice Shelf |
op_source |
EPIC3Antarctic Glaciology workshop, Norsk Polar Institutt, Tromsø |
op_relation |
Hofstede, C. orcid:0000-0002-6015-6918 , Diez, A. , Eisen, O. orcid:0000-0002-6380-962X and Kristoffersen, Y. (2011) Seismics on Ice , Antarctic Glaciology workshop, Norsk Polar Institutt, Tromsø . hdl:10013/epic.38314 |
_version_ |
1766032347418853376 |