Upper mantle structure of central and West Antarctica from array analysis of Rayleigh wave phase velocities-Reference-Cited by-同舟云学术

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

Published:2016-03 Issue:3 Volume:121 Page:1758-1775
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res. Solid Earth

Author:

Heeszel David S.¹²,Wiens Douglas A.¹,Anandakrishnan Sridhar³,Aster Richard C.⁴,Dalziel Ian W. D.⁵,Huerta Audrey D.⁶,Nyblade Andrew A.³,Wilson Terry J.⁷,Winberry J. Paul⁶

Affiliation:

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

2. United States Nuclear Regulatory Commission Washington District of Columbia 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

Funder

NSF

NSF Division of Polar Programs

DOE National Nuclear Security Administration

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/10.1002/2015JB012616

Reference114 articles.

1. Upper mantle seismic anisotropy beneath the West Antarctic Rift System and surrounding region from shear wave splitting analysis

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

3. CASERTZ aeromagnetic data reveal late Cenozoic flood basalts(?) in the West Antarctic rift system

4. Piecewise delamination of Moroccan lithosphere from beneath the Atlas Mountains

5. Active volcanism beneath the West Antarctic ice sheet and implications for ice-sheet stability

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