Distribution of oceanic crust in the Enderby Basin offshore East Antarctica

SUMMARY Seismic reflection and refraction data were collected in 2007 and 2012 to reveal the crustal fabric on a single long composite profile offshore Prydz Bay, East Antarctica. A P-wave velocity model provides insights on the crustal fabric, and a gravity-constrained density model is used to desc...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Altenbernd-Lang, Tabea, Jokat, Wilfried, Leitchenkov, German L
Other Authors: Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research
Format: Article in Journal/Newspaper
Language:English
Published: Oxford University Press (OUP) 2022
Subjects:
Geochemistry and Petrology
Geophysics
East Antarctica
Kerguelen
Prydz Bay
Antarc*
Antarctica
Online Access:http://dx.doi.org/10.1093/gji/ggac299
https://academic.oup.com/gji/advance-article-pdf/doi/10.1093/gji/ggac299/45512738/ggac299.pdf
https://academic.oup.com/gji/article-pdf/231/3/1959/45809048/ggac299.pdf
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Summary:SUMMARY Seismic reflection and refraction data were collected in 2007 and 2012 to reveal the crustal fabric on a single long composite profile offshore Prydz Bay, East Antarctica. A P-wave velocity model provides insights on the crustal fabric, and a gravity-constrained density model is used to describe the crustal and mantle structure. The models show that a 230-km-wide continent–ocean transition separates stretched continental from oceanic crust along our profile. While the oceanic crust close to the continent–ocean boundary is just 3.5–5 km thick, its thickness increases northwards towards the Southern Kerguelen Plateau to 12 km. This change is accompanied by thickening of a lower crustal layer with high P-wave velocities of up to 7.5 km s–1, marking intrusive rocks emplaced beneath the mid-ocean ridge under increasing influence of the Kerguelen plume. Joint interpretations of our crustal model, seismic reflection data and magnetic data sets constrain the age and extent of oceanic crust in the research area. Oceanic crust is shown to continue to around 160 km farther south than has been interpreted in previous data, with profound implications for plate kinematic models of the region. Finally, by combining our findings with a regional magnetic data compilation and regional seismic reflection data we propose a larger extent of oceanic crust in the Enderby Basin than previously known.

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