A seismic transect across West Antarctica: Evidence for mantle thermal anomalies beneath the Bentley Subglacial Trench and the Marie Byrd Land Dome-Reference-Cited by-同舟云学术

A seismic transect across West Antarctica: Evidence for mantle thermal anomalies beneath the Bentley Subglacial Trench and the Marie Byrd Land Dome

Published:2015-12 Issue:12 Volume:120 Page:8439-8460
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Lloyd Andrew J.¹,Wiens Douglas A.¹,Nyblade Andrew A.²,Anandakrishnan Sridhar²,Aster Richard C.³,Huerta Audrey D.⁴,Wilson Terry J.⁵,Dalziel Ian W. D.⁶,Shore Patrick J.¹,Zhao Dapeng⁷

Affiliation:

1. Department of Earth and Planetary Sciences Washington University in St. Louis St. Louis Missouri USA

2. Department of Geosciences Pennsylvania State University University Park Pennsylvania USA

3. Department of Geosciences Colorado State University Fort Collins Colorado USA

4. Department of Geological Sciences Central Washington University Ellensburg Washington USA

5. Byrd Polar Research Center and School of Earth Sciences Ohio State University Columbus Ohio USA

6. Institute for Geophysics, Jackson School of Geosciences University of Texas at Austin Austin Texas USA

7. Department of Geophysics Tohoku University Sendai Japan

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

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

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015JB012455

Reference102 articles.

1. Computations of the viscoelastic response of a 3-D compressible Earth to surface loading: an application to Glacial Isostatic Adjustment in Antarctica and Canada

2. Thermal expansivity and elastic properties of the lithospheric mantle: results from mineral physics of composites

3. Determination of three-dimensional velocity anomalies under a seismic array using first P arrival times from local earthquakes: 1. A homogeneous initial model

4. Water-Pressure Coupling of Sliding and Bed Deformation: I. Water System

5. S -velocity model and inferred Moho topography beneath the Antarctic Plate from Rayleigh waves

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