Widespread Exposures of Extensive Clean Shallow Ice in the Midlatitudes of Mars-Reference-Cited by-同舟云学术

Widespread Exposures of Extensive Clean Shallow Ice in the Midlatitudes of Mars

Published:2021-03 Issue:3 Volume:126 Page:
ISSN:2169-9097
Container-title:Journal of Geophysical Research: Planets
language:en
Short-container-title:J Geophys Res Planets

Author:

Dundas Colin M.¹^ORCID,Mellon Michael T.²,Conway Susan J.³^ORCID,Daubar Ingrid J.⁴,Williams Kaj E.¹^ORCID,Ojha Lujendra⁵,Wray James J.⁶^ORCID,Bramson Ali M.⁷^ORCID,Byrne Shane⁸^ORCID,McEwen Alfred S.⁸,Posiolova Liliya V.⁹,Speth Gunnar⁹,Viola Donna¹⁰,Landis Margaret E.¹¹^ORCID,Morgan Gareth A.¹²,Pathare Asmin V.¹²^ORCID

Affiliation:

1. U.S. Geological Survey, Astrogeology Science Center Flagstaff AZ USA

2. Center for Astrophysics and Planetary Science Cornell University Ithaca NY USA

3. Laboratoire de Planétologie et Géodynamique CNRS UMR 6112 Université de Nantes Nantes France

4. Department of Earth, Environmental, and Planetary Sciences Brown University Providence RI USA

5. Department of Earth and Planetary Sciences Rutgers University Piscataway NJ USA

6. School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta GA USA

7. Department of Earth, Atmospheric, and Planetary Sciences Purdue University West Lafayette IN USA

8. Lunar and Planetary Laboratory The University of Arizona Tucson AZ USA

9. Malin Space Science Systems San Diego CA USA

10. NASA Ames Research Center Moffett Field CA USA

11. Laboratory for Atmospheric and Space Physics University of Colorado Boulder CO USA

12. Planetary Science Institute Tucson AZ USA

Funder

National Aeronautics and Space Administration

Centre National d’Etudes Spatiales

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/10.1029/2020JE006617

Reference126 articles.

1. Winter and spring evolution of northern seasonal deposits on Mars from OMEGA on Mars Express

2. Formation of coarse sediment lags in ice-sediment mixtures: A geomorphic signature of sublimation on regolith surfaces

3. High-resolution subsurface water-ice distributions on Mars

4. Martian high latitude permafrost depth and surface cover thermal inertia distributions

5. The quantitative relationship between small impact crater morphology and regolith depth

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