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Upper mantle structure of central and West Antarctica from array analysis of Rayleigh wave phase velocities

Journal Article · · Journal of Geophysical Research. Solid Earth
DOI:https://doi.org/10.1002/2015JB012616· OSTI ID:1785806
 [1];  [2];  [3];  [4];  [5];  [6];  [3];  [7];  [6]
  1. Department of Earth and Planetary Sciences Washington University St. Louis Missouri USA, United States Nuclear Regulatory Commission Washington District of Columbia USA
  2. Department of Earth and Planetary Sciences Washington University St. Louis Missouri USA
  3. Department of Geosciences Pennsylvania State University University Park Pennsylvania USA
  4. Geosciences Department, Warner College of Natural Resources Colorado State University Fort Collins Colorado USA
  5. Institute for Geophysics University of Texas at Austin Austin Texas USA
  6. Department of Geological Sciences Central Washington University Ellensburg Washington USA
  7. Department of Geological Sciences Ohio State University Columbus Ohio USA
Abstract

The seismic velocity structure of Antarctica is important, both as a constraint on the tectonic history of the continent and for understanding solid Earth interactions with the ice sheet. We use Rayleigh wave array analysis methods applied to teleseismic data from recent temporary broadband seismograph deployments to image the upper mantle structure of central and West Antarctica. Phase velocity maps are determined using a two–plane wave tomography method and are inverted for shear velocity using a Monte Carlo approach to estimate three‐dimensional velocity structure. Results illuminate the structural dichotomy between the East Antarctic Craton and West Antarctica, with West Antarctica showing thinner crust and slower upper mantle velocity. West Antarctica is characterized by a 70–100 km thick lithosphere, underlain by a low‐velocity zone to depths of at least 200 km. The slowest anomalies are beneath Ross Island and the Marie Byrd Land dome and are interpreted as upper mantle thermal anomalies possibly due to mantle plumes. The central Transantarctic Mountains are marked by an uppermost mantle slow‐velocity anomaly, suggesting that the topography is thermally supported. The presence of thin, higher‐velocity lithosphere to depths of about 70 km beneath the West Antarctic Rift System limits estimates of the regionally averaged heat flow to less than 90 mW/m 2 . The Ellsworth‐Whitmore block is underlain by mantle with velocities that are intermediate between those of the West Antarctic Rift System and the East Antarctic Craton. We interpret this province as Precambrian continental lithosphere that has been altered by Phanerozoic tectonic and magmatic activity.

Sponsoring Organization:
USDOE National Nuclear Security Administration (NNSA)
OSTI ID:
1785806
Journal Information:
Journal of Geophysical Research. Solid Earth, Journal Name: Journal of Geophysical Research. Solid Earth Journal Issue: 3 Vol. 121; ISSN 2169-9313
Publisher:
American Geophysical Union (AGU)Copyright Statement
Country of Publication:
United States
Language:
English

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