Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy-Reference-Cited by-同舟云学术

Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy

Published:2022-09-15 Issue:18 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Ben‐Mansour Walid¹^ORCID,Wiens Douglas A.¹^ORCID,Mark Hannah F.¹²^ORCID,Russo Raymond M.³^ORCID,Richter Andreas⁴^ORCID,Marderwald Eric⁴^ORCID,Barrientos Sergio⁵

Affiliation:

1. Department of Earth & Planetary Sciences Washington University in Saint Louis Saint Louis MO USA

2. Woods Hole Oceanographic Institution Woods Hole MA USA

3. Department of Geological Sciences University of Florida Gainesville FL USA

4. Laboratorio MAGGIA Universidad Nacional de La Plata CONICET La Plata Argentina

5. Centro Sismológico Nacional Universidad de Chile Santiago Chile

Funder

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL099871

Reference46 articles.

1. Geologically current motion of 56 plates relative to the no-net-rotation reference frame

2. Heat flow and lithospheric thickness analysis in the Patagonian asthenospheric windows, southern South America

3. Anisotropy patterns in the subducting lithosphere and in the mantle wedge: A case study—The southern Italy subduction system

4. Neogene kinematic history of Nazca–Antarctic–Phoenix slab windows beneath Patagonia and the Antarctic Peninsula

5. Multichannel analysis of shear wave splitting

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