A cold-wet middle-latitude environment on Mars during the Hesperian-Amazonian transition: Evidence from northern Arabia valleys and paleolakes-Reference-Cited by-同舟云学术

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A cold-wet middle-latitude environment on Mars during the Hesperian-Amazonian transition: Evidence from northern Arabia valleys and paleolakes

Published:2016-09 Issue:9 Volume:121 Page:1667-1694
ISSN:2169-9097
Container-title:Journal of Geophysical Research: Planets
language:en
Short-container-title:J. Geophys. Res. Planets

Author:

Wilson Sharon A.¹²,Howard Alan D.²,Moore Jeffrey M.³,Grant John A.¹

Affiliation:

1. Center for Earth and Planetary Studies, National Air and Space Museum; Smithsonian Institution; Washington District of Columbia USA

2. Department of Environmental Sciences; University of Virginia; Charlottesville Virginia USA

3. NASA Ames Research Center, Space Sciences Division; Moffett Field California USA

Funder

NASA

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016JE005052/fullpdf

Reference88 articles.

1. Amazonian-aged fluvial system and associated ice-related features in Terra Cimmeria, Mars;Adeli;Icarus,2016

2. Early Mars hydrology: Meridiani playa deposits and the sedimentary record of Arabia Terra;Andrews-Hanna;J. Geophys. Res.,2010

3. New observations of Warrego Valles, Mars: Evidence for precipitation and surface runoff;Ansan;Planet. Space Sci.,2006

4. Degradation of mid-latitude craters on Mars;Berman;Icarus,2009

5. Tundra lakes and permafrost, Richards Island, western Arctic coast, Canada;Burn;Can. J. Earth Sci.,2002

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