Sulfur Cycling in Gypsum Dunes from New Mexico - Terrestrial Analogs to Sulphate-Eolian Deposition and Early Diagenesis on Mars. Preliminary Results.

Szynkiewicz A, Pratt LM, Glamoclija M. 2007. Sulfur Cycling in Gypsum Dunes from New Mexico - Terrestrial Analogs to Sulphate-Eolian Deposition and Early Diagenesis on Mars. Preliminary Results.. Indiana University, Department of Geological Sciences. Bloomington, IN

Research for this study occurred at White Sands National Monument. Preliminary results show that sulfate eolian deposits from the Salt Basins associated with the Rio Grande Rift evolution are competitive places for astrobiological constrains, climate and sulfur studies in order to better understand Martian sulfur cycle and climate evolution.

Type
Unpublished Report
Authors
Szynkiewicz, A.; Pratt, L.; Glamoclija, M.
Date of Issue
2007
Publisher
Indiana University, Department of Geological Sciences
Units
WHSA
Keywords
Atmospheric Sciences, Climate, gypsum dunes, Mars, Physical Sciences, Sulfur

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