Mineralogy and aqueous alteration martian surface
Listed on 2025-12-29
-
Science
Research Scientist, Environmental Science -
Research/Development
Research Scientist
Mineralogy and aqueous alteration of the martian surface
Join to apply for the Mineralogy and aqueous alteration of the martian surface role at ORAU
OrganizationNational Aeronautics and Space Administration (NASA)
Reference Code0012-NPP-MAR
26-JSC-Planet Sci
All applications must be submitted in Zintellect.
Please visit the NASA Postdoctoral Program website for application instructions and requirements:
How to Apply
| NASA Postdoctoral Program (orau.org).
A complete application to the NASA Postdoctoral Program includes:
- Research proposal
- Three letters of recommendation
- Official doctoral transcript documents
3/1/2026 6:00:59 PM Eastern Time Zone
DescriptionAbout the NASA Postdoctoral Program The NASA Postdoctoral Program (NPP) offers unique research opportunities to highly-talented scientists to engage in ongoing NASA research projects at a NASA Center, NASA Headquarters, or at a NASA-affiliated research institute. These one- to three-year fellowships are competitive and are designed to advance NASA’s missions in space science, Earth science, aeronautics, space operations, exploration systems, and astrobiology.
Description: Surface mineralogy and geochemistry of Mars are key to characterizing geological processes on ancient and modern Mars. Mineralogical and geochemical measurements from Mars show that the ancient surface was altered by liquid water. The types of minerals and geochemical trends observed on the surface can help determine the characteristics of these ancient aqueous environments and whether or not they would have been habitable to microbial life.
The goal of this research is to reconstruct the history of liquid water on Mars through mineralogical and geochemical measurements of the martian surface and analog materials. These analog materials can be synthesized in the laboratory or collected from Mars analog sites on Earth. Studies of phyllosilicate, iron oxide, sulfate, and carbonate minerals and amorphous or poorly crystalline phases are encouraged.
Studies of mineral sorting and segregation in fluviolacustrine and aeolian environments on Earth as a means to interpret the mineralogy of martian surface deposits are also of great interest.
Analytical instruments available at JSC include X-ray diffraction, infrared spectroscopy, thermal and evolved gas analysis, laser-induced breakdown spectroscopy, ion chromatography, scanning electron microscopy, transmission electron microscopy, and electron microprobe. JSC also has test bed instruments for the Che Min X-ray diffractometer on the Mars Science Laboratory Curiosity rover, the Sample Analysis at Mars (SAM) instrument on Curiosity, the Thermal and Evolved Gas Analyzer (TEGA) on Phoenix, Chem Cam on Curiosity, and the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) on the Mars Reconnaissance Orbiter, and data collected on these instruments are directly comparable to those collected on Mars.
Scientists with experience analyzing weathering products or amorphous materials using Synchrotron techniques are also encouraged to apply.
References:
Rampe,
E.
B., R. V. Morris, P.
D. Archer Jr.,
D. G. Agresti,
D. W. Ming (2016) Recognizing sulfate and phosphate complexes chemisorbed onto nanophase weathering products on Mars using in-situ and remote observations. American Mineralogist, 101(3), 678-689, doi:
10.2138/am-CCBYNCND.
Rampe,
E.
B., M.
D. Kraft, T. G. Sharp,
D.
C. Golden,
D. W. Ming, P. R. Christensen (2012) Allophane detection on Mars with Thermal Emission Spectrometer data and implications for regional-scale chemical weathering processes. Geology, 40(11), 995-998, doi:
10.1130/G33215.1.
Rampe,
E.
B.,
D. W. Ming, J. P. Grotzinger, R. V. Morris,
D.
F. Blake,
D. T. Vaniman, T.
F. Bristow, S. M. Morrison,
A. S. Yen, S. J. Chipera, R. T. Downs,
C. N. Achilles, R. M. Hazen, T. S. Peretyazhko,
B. Sutter,
A. H. Treiman, P. I. Craig, J.
D. Farmer,
D. J. Des Marais,
A. G. Fairén (2017) Mineral trends in early Hesperian lacustrine mudstone at Gale crater, Mars. LPS XLVII, 2821.
Rampe,
E.
B.,
B. Horgan, N. Scudder, R. J. Smith,
A. M. Rutledge (2017) Mineralogy of rock flour in glaciated volcanic terrains:
A…
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