Active geophysics on Ekströmisen and Halfvarryggen, Antarctica
Halfvarryggen is a small ice dome bordering the catchment area of Ekströmisen. It is a candidate for drilling one IPICS 2k/40k ice core. Near the actual dome, three ice divides merge in a triple point. Halvfarryggens internal structure has been imaged with airborne radio-echo sounding (RES) in the p...
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ftawi:oai:epic.awi.de:22271 2023-05-15T13:46:50+02:00 Active geophysics on Ekströmisen and Halfvarryggen, Antarctica Eisen, Olaf Blenkner, R. Diez, Anja Drews, Reinhard Hofstede, Coen Kristoffersen, Y. Jansen, Daniela Lambrecht, A. Mayer, Christoph Neckel, Niklas Steinhage, Daniel Witt, Ralf 2010 application/pdf https://epic.awi.de/id/eprint/22271/ https://epic.awi.de/id/eprint/22271/1/Eis2010b.pdf https://hdl.handle.net/10013/epic.34574 https://hdl.handle.net/10013/epic.34574.d001 unknown https://epic.awi.de/id/eprint/22271/1/Eis2010b.pdf https://hdl.handle.net/10013/epic.34574.d001 Eisen, O. orcid:0000-0002-6380-962X , Blenkner, R. , Diez, A. , Drews, R. , Hofstede, C. orcid:0000-0002-6015-6918 , Kristoffersen, Y. , Jansen, D. orcid:0000-0002-4412-5820 , Lambrecht, A. , Mayer, C. , Neckel, N. orcid:0000-0003-4300-5488 , Steinhage, D. orcid:0000-0003-4737-9751 and Witt, R. (2010) Active geophysics on Ekströmisen and Halfvarryggen, Antarctica , EGU General Assembly, 02.-07. May, Vienna, Austria. . hdl:10013/epic.34574 EPIC3EGU General Assembly, 02.-07. May, Vienna, Austria. Conference notRev 2010 ftawi 2021-12-24T15:34:10Z Halfvarryggen is a small ice dome bordering the catchment area of Ekströmisen. It is a candidate for drilling one IPICS 2k/40k ice core. Near the actual dome, three ice divides merge in a triple point. Halvfarryggens internal structure has been imaged with airborne radio-echo sounding (RES) in the past years, which indicate upwarping internal layers, so-called isochrone arches (or partly Raymond bumps), which develop into a double bump at larger depths. Modelling studies (Martin et al., 2009, JGR-F) indicate that the crystal orientation fabric (COF) at larger depths at ice domes like Halvfarryggen should be highly anisotropic. As changes in COF not only change the dielectric permittivity, but also the acoustic impedance contrast, such changes should also be detectable with seismic methods. We present an overview and preliminary results of a geophysical LIMPICS campaign at Halfvarryggen in 2009/10, involving reflection seismics, shallow ground-penetrating radar (GPR) and other glaciological studies. Main scientific goals were to detect internal reflection horizons along a profile nearby the ice dome with seismics and GPR, image the internal layer architecture along hexagons crossing all three ice divides, detect the ice-bed interface and image the upper tens of meters of the underlying bedrock. Conference Object Antarc* Antarctica ice core Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Ekströmisen ENVELOPE(-8.000,-8.000,-71.000,-71.000) Halvfarryggen ENVELOPE(-6.500,-6.500,-71.167,-71.167) |
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Open Polar |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
op_collection_id |
ftawi |
language |
unknown |
description |
Halfvarryggen is a small ice dome bordering the catchment area of Ekströmisen. It is a candidate for drilling one IPICS 2k/40k ice core. Near the actual dome, three ice divides merge in a triple point. Halvfarryggens internal structure has been imaged with airborne radio-echo sounding (RES) in the past years, which indicate upwarping internal layers, so-called isochrone arches (or partly Raymond bumps), which develop into a double bump at larger depths. Modelling studies (Martin et al., 2009, JGR-F) indicate that the crystal orientation fabric (COF) at larger depths at ice domes like Halvfarryggen should be highly anisotropic. As changes in COF not only change the dielectric permittivity, but also the acoustic impedance contrast, such changes should also be detectable with seismic methods. We present an overview and preliminary results of a geophysical LIMPICS campaign at Halfvarryggen in 2009/10, involving reflection seismics, shallow ground-penetrating radar (GPR) and other glaciological studies. Main scientific goals were to detect internal reflection horizons along a profile nearby the ice dome with seismics and GPR, image the internal layer architecture along hexagons crossing all three ice divides, detect the ice-bed interface and image the upper tens of meters of the underlying bedrock. |
format |
Conference Object |
author |
Eisen, Olaf Blenkner, R. Diez, Anja Drews, Reinhard Hofstede, Coen Kristoffersen, Y. Jansen, Daniela Lambrecht, A. Mayer, Christoph Neckel, Niklas Steinhage, Daniel Witt, Ralf |
spellingShingle |
Eisen, Olaf Blenkner, R. Diez, Anja Drews, Reinhard Hofstede, Coen Kristoffersen, Y. Jansen, Daniela Lambrecht, A. Mayer, Christoph Neckel, Niklas Steinhage, Daniel Witt, Ralf Active geophysics on Ekströmisen and Halfvarryggen, Antarctica |
author_facet |
Eisen, Olaf Blenkner, R. Diez, Anja Drews, Reinhard Hofstede, Coen Kristoffersen, Y. Jansen, Daniela Lambrecht, A. Mayer, Christoph Neckel, Niklas Steinhage, Daniel Witt, Ralf |
author_sort |
Eisen, Olaf |
title |
Active geophysics on Ekströmisen and Halfvarryggen, Antarctica |
title_short |
Active geophysics on Ekströmisen and Halfvarryggen, Antarctica |
title_full |
Active geophysics on Ekströmisen and Halfvarryggen, Antarctica |
title_fullStr |
Active geophysics on Ekströmisen and Halfvarryggen, Antarctica |
title_full_unstemmed |
Active geophysics on Ekströmisen and Halfvarryggen, Antarctica |
title_sort |
active geophysics on ekströmisen and halfvarryggen, antarctica |
publishDate |
2010 |
url |
https://epic.awi.de/id/eprint/22271/ https://epic.awi.de/id/eprint/22271/1/Eis2010b.pdf https://hdl.handle.net/10013/epic.34574 https://hdl.handle.net/10013/epic.34574.d001 |
long_lat |
ENVELOPE(-8.000,-8.000,-71.000,-71.000) ENVELOPE(-6.500,-6.500,-71.167,-71.167) |
geographic |
Ekströmisen Halvfarryggen |
geographic_facet |
Ekströmisen Halvfarryggen |
genre |
Antarc* Antarctica ice core |
genre_facet |
Antarc* Antarctica ice core |
op_source |
EPIC3EGU General Assembly, 02.-07. May, Vienna, Austria. |
op_relation |
https://epic.awi.de/id/eprint/22271/1/Eis2010b.pdf https://hdl.handle.net/10013/epic.34574.d001 Eisen, O. orcid:0000-0002-6380-962X , Blenkner, R. , Diez, A. , Drews, R. , Hofstede, C. orcid:0000-0002-6015-6918 , Kristoffersen, Y. , Jansen, D. orcid:0000-0002-4412-5820 , Lambrecht, A. , Mayer, C. , Neckel, N. orcid:0000-0003-4300-5488 , Steinhage, D. orcid:0000-0003-4737-9751 and Witt, R. (2010) Active geophysics on Ekströmisen and Halfvarryggen, Antarctica , EGU General Assembly, 02.-07. May, Vienna, Austria. . hdl:10013/epic.34574 |
_version_ |
1766245293116882944 |