Crustal Anisotropy in the Martian Lowlands From Surface Waves-Reference-Cited by-同舟云学术

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Crustal Anisotropy in the Martian Lowlands From Surface Waves

Published:2022-12-14 Issue:24 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Beghein C.¹^ORCID,Li J.¹^ORCID,Weidner E.¹,Maguire R.²^ORCID,Wookey J.³^ORCID,Lekić V.⁴^ORCID,Lognonné P.⁵^ORCID,Banerdt W.⁶^ORCID

Affiliation:

1. Department of Earth, Planetary, and Space Sciences University of California Los Angeles Los Angeles CA USA

2. Department of Geology University of Illinois Urbana‐Champaign Urbana IL USA

3. School of Earth Sciences University of Bristol Bristol UK

4. Department of Geology University of Maryland College Park MD USA

5. CNRS Institut de physique du globe de Paris Université Paris Cité Paris France

6. Jet Propulsion Laboratory California Institute of Technology Pasadena CA USA

Funder

Planetary Science Division

Centre National d'Etudes Spatiales

Agence Nationale de la Recherche

UK Space Agency

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL101508

Reference70 articles.

1. Elastic wave propagation in layered anisotropic media

2. The Borealis basin and the origin of the martian crustal dichotomy

3. Long-wave elastic anisotropy produced by horizontal layering

4. Initial results from the InSight mission on Mars

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4. Structure of the Martian Crust Below InSight From Surface Waves and Body Waves Generated by Nearby Meteoroid Impacts;Geophysical Research Letters;2023-11-29

5. Martian Crustal Model From a Joint Inversion of Receiver Functions and Apparent Shear Wave Velocity;Journal of Geophysical Research: Planets;2023-11

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