Seismic reflection constraints on the glacial dynamics of Johnsons Glacier,Antarctica |
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| Institution: | 2. Duke University, Durham, NC, United States;3. University of Montana, Missoula, MT, United States;4. Virginia Tech, Blacksburg, VA, United States;5. Aquatic Analysis and Consulting LLC, Morehead City, NC, United States;1. Department of Civil Engineering, University of Minho Portugal, Campus de Azurém, 4800-058 Guimarães, Portugal;2. Laboratório de Planejamento e Projetos, UFES, Brasil, Av. Fernando Ferrari, 514, Room 7, Vitória - Espírito Santo 29075-910, Brazil |
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| Abstract: | During two Antarctic summers (1996–1997 and 1997–1998), five seismic refraction and two reflection profiles were acquired on the Johnsons Glacier (Livingston Island, Antarctica) in order to obtain information about the structure of the ice, characteristics of the ice-bed contact and basement topography. An innovative technique has been used for the acquisition of reflection data to optimise the field survey schedule. Different shallow seismic sources were used during each field season: Seismic Impulse Source System (SISSY) for the first field survey and low-energy explosives (pyrotechnic noisemakers) during the second one. A comparison between these two shallow seismic sources has been performed, showing that the use of the explosives is a better seismic source in this ice environment. This is one of the first studies where this type of source has been used. The analysis of seismic data corresponding to one of the reflection profiles (L3) allows us to delineate sectors with different glacier structure (accumulation and ablation zones) without using glaciological data. Moreover, vertical discontinuities were detected by the presence of back-scattered energy and the abrupt change in frequency content of first arrivals shown in shot records. After the raw data analysis, standard processing led us to a clear seismic image of the underlying bed topography, which can be correlated with the ice flow velocity anomalies. The information obtained from seismic data on the internal structure of the glacier, location of fracture zones and the topography of the ice-bed interface constrains the glacial dynamics of Johnsons Glacier. |
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