New observations of martian southern mid-latitude recurring slope lineae (RSL) imply formation by freshwater subsurface flows-Reference-Cited by-同舟云学术

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New observations of martian southern mid-latitude recurring slope lineae (RSL) imply formation by freshwater subsurface flows

Published:2014-05 Issue: Volume:233 Page:328-341
ISSN:0019-1035
Container-title:Icarus
language:en
Short-container-title:Icarus

Author:

Stillman David E.,Michaels Timothy I.,Grimm Robert E.,Harrison Keith P.

Funder

NASA Mars Fundamental Research Program

Publisher

Elsevier BV

Subject

Space and Planetary Science,Astronomy and Astrophysics

Reference49 articles.

1. Experimental investigation of the stability and evaporation of sulfate and chloride brines on Mars;Altheide;Earth Planet. Sci. Lett.,2009

2. Stability of ice on Mars and the water vapor diurnal cycle: Experimental study of the sublimation of ice through a fine-grained basaltic regolith;Bryson;Icarus,2008

3. Formation of recurring slope lineae by liquid brines on present-day Mars;Chevrier;Geophys. Res. Lett.,2012

4. The sublimation rate of ice under simulated Mars conditions and the effect of layers of mock regolith JSC Mars-1;Chevrier;Geophys. Res. Lett.,2007

5. Experimental study of the sublimation of ice through an unconsolidated clay layer: Implications for the stability of ice on Mars and the possible diurnal variations in atmospheric water;Chevrier;Icarus,2008

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