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Auteurs principaux: Hofstede, Coen Matthijs, Schlegel, Rebecca, Diez, Anja, Freitag, Johannes, Lambrecht, Astrid, Mayer, Christoph, Miller, Heinrich, Eisen, Olaf
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 2021
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Accès en ligne:https://doi.org/10.1594/PANGAEA.932774
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author Hofstede, Coen Matthijs
Schlegel, Rebecca
Diez, Anja
Freitag, Johannes
Lambrecht, Astrid
Mayer, Christoph
Miller, Heinrich
Eisen, Olaf
author_facet Hofstede, Coen Matthijs
Schlegel, Rebecca
Diez, Anja
Freitag, Johannes
Lambrecht, Astrid
Mayer, Christoph
Miller, Heinrich
Eisen, Olaf
collection Datos científicos de ciencias marinas y ambientales
contents In 2012 we performed an active seismic experiment at Kohnen Station, (S 75.0041, E 0.0637), Antarctica. We recorded two perpendicular seismic profiles. The source was a minivibrator (ELVIS, wheelbarrow sized) producing a 30-240 Hz, 10 s linear sweep. The receivers were 24 3-component spiked geophones place at 10 m (parallel line 20120553) or 5 m separation (perpendicular line 20120554). The first arrivals from the diving wave of the correlated sweep records were used to derive elastic modeli from the firn. We present the raw uncorrelated sweeps, the correlated sweeps and stacks used in the publication Schlegel, R. et al. (2019).
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_932774
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle Three component shallow seismic mini-vibrator data of polar firn of Kohnen Station, East Antarctica
Hofstede, Coen Matthijs
Schlegel, Rebecca
Diez, Anja
Freitag, Johannes
Lambrecht, Astrid
Mayer, Christoph
Miller, Heinrich
Eisen, Olaf
20120553, 20120554; Binary Object; Binary Object (File Size); Comment; diving wave; East Antarctica, Kohnen station; File content; firn; Kohnen_based; Kohnen_seismic_2012; Kohnen Station; p-wave; SEIS; Seismic; s-wave; vibroseis
In 2012 we performed an active seismic experiment at Kohnen Station, (S 75.0041, E 0.0637), Antarctica. We recorded two perpendicular seismic profiles. The source was a minivibrator (ELVIS, wheelbarrow sized) producing a 30-240 Hz, 10 s linear sweep. The receivers were 24 3-component spiked geophones place at 10 m (parallel line 20120553) or 5 m separation (perpendicular line 20120554). The first arrivals from the diving wave of the correlated sweep records were used to derive elastic modeli from the firn. We present the raw uncorrelated sweeps, the correlated sweeps and stacks used in the publication Schlegel, R. et al. (2019).
title Three component shallow seismic mini-vibrator data of polar firn of Kohnen Station, East Antarctica
topic 20120553, 20120554; Binary Object; Binary Object (File Size); Comment; diving wave; East Antarctica, Kohnen station; File content; firn; Kohnen_based; Kohnen_seismic_2012; Kohnen Station; p-wave; SEIS; Seismic; s-wave; vibroseis
url https://doi.org/10.1594/PANGAEA.932774