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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Bibliographic Details
Main Authors: Hofstede, Coen, Diez, Anja, Eisen, Olaf, Kristoffersen, Y.
Format: Conference Object
Language:unknown
Published: 2011
Subjects:
Ice Shelf
Online Access:https://epic.awi.de/id/eprint/25144/
https://hdl.handle.net/10013/epic.38314
id ftawi:oai:epic.awi.de:25144
record_format openpolar
spelling 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)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language 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
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