Measuring Ripple and Dune Migration in Coprates Chasma, Valles Marineris: A Source to Sink Aeolian System on Mars?-Reference-Cited by-同舟云学术

Measuring Ripple and Dune Migration in Coprates Chasma, Valles Marineris: A Source to Sink Aeolian System on 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:

Boazman S. J.¹²^ORCID,Davis J. M.¹^ORCID,Grindrod P. M.¹^ORCID,Balme M. R.³^ORCID,Vermeesch P.²,Baird T.²^ORCID

Affiliation:

1. Department of Earth Sciences Natural History Museum London UK

2. Department of Earth Sciences University College London London UK

3. Department of Physical Sciences Open University Milton Keynes UK

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/10.1029/2020JE006608

Reference61 articles.

1. The formation of Valles Marineris: 3. Trough formation through super‐isostasy, stress, sedimentation, and subsidence;Andrews‐Hanna J. C.;Journal of Geophysical Research,2012

2. Threshold for sand mobility on Mars calibrated from seasonal variations of sand flux

3. Measuring Sand Dune Migration Rates with COSI-Corr and Landsat: Opportunities and Challenges

4. Ancient Martian aeolian processes and palaeomorphology reconstructed from the Stimson formation on the lower slope of Aeolis Mons, Gale crater, Mars

5. Patterns in Mobility and Modification of Middle- and High-Latitude Southern Hemisphere Dunes on Mars

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