2010
DOI: 10.1016/j.epsl.2010.10.022
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Crustal structure of the Gamburtsev Mountains, East Antarctica, from S-wave receiver functions and Rayleigh wave phase velocities

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Cited by 77 publications
(100 citation statements)
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“…The velocity used here is reasonable given that it is in the general range of ice determined by seismic experiments (Kim et al, 2010). Moreover, this velocity has also been widely used in previous studies (Hansen et al, 2010;Wittlinger and Farra, 2012;Ramirez et al, 2016). Keeping the velocities set, the ice thickness at each station was then calculated using Eq.…”
Section: Methodsmentioning
confidence: 99%
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“…The velocity used here is reasonable given that it is in the general range of ice determined by seismic experiments (Kim et al, 2010). Moreover, this velocity has also been widely used in previous studies (Hansen et al, 2010;Wittlinger and Farra, 2012;Ramirez et al, 2016). Keeping the velocities set, the ice thickness at each station was then calculated using Eq.…”
Section: Methodsmentioning
confidence: 99%
“…Over the past two decades, several temporary seismic arrays have been deployed in Antarctica, including the TransAntarctic Mountains Seismic Experiment (TAMSEIS, 2000(TAMSEIS, -2003 (Lawrence et al, 2006), the Gamburtsev Antarctic Mountains Seismic Experiment (GAMSEIS, 2007(GAMSEIS, -2012 (Hansen et al, 2010) and the Polar Earth Observing Network/Antarctic Network (POLENET/ANET, 2007-2016) (Chaput et al, 2014). Despite their relatively sparse distribution compared to many dense seismic arrays on other continents, these three arrays combined effectively cover East and West Antarctica as well as the Transantarctic Mountains region (Fig.…”
Section: Datamentioning
confidence: 99%
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“…In Antarctica, the most ambitious seismological field campaign conducted for the IPY was the «GAmburtsev Mountain SEISmic experiment» or GAMSEIS, an internationally coordinated deployment of more than 50 broadband seismographs over the crest of the Gambursev Mountains (Dome-A -Dome-F area) in East Antarctica. The aim of this experiment was to provide detailed information on the crustal thickness and mantle structure of the region and find key constraints on the origin of the Gamburtsev Mountains (Wiens, 2007;Hansen et al, 2010;. GAMSEIS and many other seismological deployments, including a French deployment between Concordia and Vostok (CASE-IPY) and a Japanese deployment around the Lützow-Holm Bay (JARE-GARNET), were coordinated under a larger program called the 'Polar Earth Observing Network (POLENET; http://www.polenet.org/; Fig.…”
Section: Greenland Ice Sheet Monitoring Network (Glisn)mentioning
confidence: 99%