2010
DOI: 10.1130/l116.1
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Gravity anomalies of the Antarctic lithosphere

Abstract: Anomalous free-air gravity signals in and around the Antarctic continent have been reported for some decades. Recent defi nition of the Antarctic gravity fi eld from fi eld-based oversnow traverses and supporting data from Earth-orbiting satellites reveal discrete regions of both negative and positive free-air gravity anomalies. The data from these observations have enabled us to construct a free-air gravity anomaly map of Antarctica. Negative free-air gravity anomalies are found to occur mainly on the Antarct… Show more

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Cited by 6 publications
(11 citation statements)
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“…Other candidates such as the giant Wilkes Land Crater have been associated with the end Permian extinction; but neither the age of that crater nor its association with the Permian–Triassic events are proven. Its location under the Antarctic ice (Weihaupt ) is a formidable barrier to any further investigation at present.…”
Section: Analysis Of the Crater Agesmentioning
confidence: 99%
“…Other candidates such as the giant Wilkes Land Crater have been associated with the end Permian extinction; but neither the age of that crater nor its association with the Permian–Triassic events are proven. Its location under the Antarctic ice (Weihaupt ) is a formidable barrier to any further investigation at present.…”
Section: Analysis Of the Crater Agesmentioning
confidence: 99%
“…6a Enlargement of the area of the subglacial topography of the Wilkes Land Anomaly (WLA) shown in Figs 4 & 5. Compiled from Victoria Land Traverse and Adélie Land Traverse ground-based gravity and seismic surveys (after Rouillon 1960, Weihaupt 1961, Weihaupt et al 2010, Weihaupt et al 2012), from airborne radiosound survey (after Steed & Drewry 1982), from airborne gravity and magnetic survey (after Ferraccioli et al 2001) and from the BEDMAP2 dataset (after Fretwell et al 2013). b. Mosaic of RADARSAT imaging of the continental ice sheet surface overlying the WLA, reflecting the subglacial morphology of the craterform structure.…”
Section: Gravity Deficitmentioning
confidence: 99%
“…The subglacial topography of both the WSB and the WLA reported by the VLT has been further confirmed by more recent investigations in the region related to the continental ice sheet, crust, lithosphere and mantle. These include airborne radiosound survey (Steed & Drewry 1982, Lythe & Vaughan 2001), airborne magnetic survey (Ferraccioli et al 2001), airborne gravity survey (Jordan et al 2014) and satellite remote sensing (Reigber et al 2002, Weihaupt et al 2010), as well as WISE/ISODYN British-Italian multidisciplinary surveys involving aeromagnetic, aerogravity, seismic, electrical conductivity and petrologic studies (Bozzo & Ferraccioli 2007). All report the subglacial topography of the WSB and the WLA to be in very good agreement with that of the original VLT ground-based survey.…”
Section: Introductionmentioning
confidence: 99%
“…A giant impact crater beneath the Wilkes Land ice sheet was first proposed by Schmidt (1962); the hypothesis was developed by Weihaupt (1976), challenged by Bentley (1979) and supported by Weihaupt (2010). The Wilkes Land anomaly or mascon was first reported by von Frese et al (2006Frese et al ( , 2009 analyzing satellite gravity data available at that time.…”
Section: Motive and Aimmentioning
confidence: 97%