Temperature, lithosphere-asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities

Meijian An, Douglas A. Wiens, Yue Zhao, Mei Feng, Andrew Arnold Nyblade, Masaki Kanao, Yuansheng Li, Alessia Maggi, Jean Jacques Lévêque

Research output: Contribution to journalArticle

30 Citations (Scopus)

Abstract

We estimate the upper mantle temperature of the Antarctic Plate based on the thermoelastic properties of mantle minerals and S velocities using a new 3-D shear velocity model, AN1-S. Crustal temperatures and surface heat fluxes are then calculated from the upper mantle temperature assuming steady state thermal conduction. The temperature at the top of the asthenosphere beneath the oceanic region and West Antarctica is higher than the dry mantle solidus, indicating the presence of melt. From the temperature values, we generate depth maps of the lithosphere-asthenosphere boundary and the Curie temperature isotherm. The maps show that East Antarctica has a thick lithosphere similar to that of other stable cratons, with the thickest lithosphere (~250 km) between Domes A and C. The thin crust and lithosphere beneath West Antarctica are similar to those of modern subduction-related rift systems in East Asia. A cold region beneath the Antarctic Peninsula is similar in spatial extent to that of a flat-subducted slab beneath the southern Andes, indicating a possible remnant of the Phoenix Plate, which was subducted prior to 10 Ma. The oceanic lithosphere generally thickens with increasing age, and the age-thickness correlation depends on the spreading rate of the ridge that formed the lithosphere. Significant flattening of the age-thickness curves is not observed for the mature oceanic lithosphere of the Antarctic Plate.

Original languageEnglish (US)
Pages (from-to)8720-8742
Number of pages23
JournalJournal of Geophysical Research: Solid Earth
Volume120
Issue number12
DOIs
StatePublished - Dec 1 2015

Fingerprint

asthenosphere
seismic velocity
lithosphere
heat flux
Heat flux
Earth mantle
Antarctic regions
temperature
oceanic lithosphere
Temperature
upper mantle
mantle
Domes
Curie temperature
cold region
Phoenix (AZ)
Minerals
Isotherms
solidus
cratons

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Geochemistry and Petrology
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science

Cite this

An, Meijian ; Wiens, Douglas A. ; Zhao, Yue ; Feng, Mei ; Nyblade, Andrew Arnold ; Kanao, Masaki ; Li, Yuansheng ; Maggi, Alessia ; Lévêque, Jean Jacques. / Temperature, lithosphere-asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities. In: Journal of Geophysical Research: Solid Earth. 2015 ; Vol. 120, No. 12. pp. 8720-8742.
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Temperature, lithosphere-asthenosphere boundary, and heat flux beneath the Antarctic Plate inferred from seismic velocities. / An, Meijian; Wiens, Douglas A.; Zhao, Yue; Feng, Mei; Nyblade, Andrew Arnold; Kanao, Masaki; Li, Yuansheng; Maggi, Alessia; Lévêque, Jean Jacques.

In: Journal of Geophysical Research: Solid Earth, Vol. 120, No. 12, 01.12.2015, p. 8720-8742.

Research output: Contribution to journalArticle

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AU - An, Meijian

AU - Wiens, Douglas A.

AU - Zhao, Yue

AU - Feng, Mei

AU - Nyblade, Andrew Arnold

AU - Kanao, Masaki

AU - Li, Yuansheng

AU - Maggi, Alessia

AU - Lévêque, Jean Jacques

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