NASA Astrobiology



A volcanically active planet is shown in closeup at the left side of the image with glowing eruptions and lines of lava on the surface. To the right and in the distance is a faint blue glowing ball representing the more massive planet in the system.

Sixteen frames from Voyager 1's flyby of Jupiter in 1979 were merged to create this image. Jupiter's Great Red Spot is visible in the center. Jupiter's moon Europa can be seen in the foreground at the bottom left of the image.

The frame is a horizontal rainbow of color on a grid. Shadows of molecules can be seen through the light as well as the jagged peaks and troughs of spectral lines.

Fizzy Super Earths and Lava Worlds“Fizzy Super-Earths: Impacts of Magma Composition on the Bulk Density and Structure of Lava Worlds.” in The Astrophysical Journal.01/03

Identifying Hydrothermal Activity on Icy Ocean Worlds“Ethene-ethanol ratios as potential indicators of hydrothermal activity at Enceladus, Europa, and other icy ocean worlds.” In Icarus.02/03

NASA Raman Spectroscopic Database"The NASA Raman spectroscopic database: Ramdb version 1.00.” In Icarus.03/03

NextPrevious

Go Explore

January 2012Raman Spectroscopy at High Pressures

Goncharov, A. F. (2012). International Journal of Spectroscopy, 2012(None), 1–16. doi:10.1155/2012/617528

P/2010 A2 LINEAR

Hainaut, O. R., Kleyna, J., Sarid, G., Hermalyn, B., Zenn, A., Meech, K. J., … Schultz, P. H. (2012). A&A, 537(None), A69. doi:10.1051/0004-6361/201118147

New light-travel time models and orbital stability study of the proposed planetary system HU Aquarii

Hinse, T. C., Lee, J. W., Goździewski, K., Haghighipour, N., Lee, C-U., & Scullion, E. M. (2012). Monthly Notices of the Royal Astronomical Society, 420(4), 3609–3620. doi:10.1111/j.1365-2966.2011.20283.x

Silician magnetite from the Dales Gorge Member of the Brockman Iron Formation, Hamersley Group, Western Australia

Huberty, J. M., Konishi, H., Heck, P. R., Fournelle, J. H., Valley, J. W., & Xu, H. (2012). American Mineralogist, 97(1), 26–37. doi:10.2138/am.2012.3864

High-pressure tolerance in Halobacterium salinarum NRC-1 and other non-piezophilic prokaryotes

Kish, A., Griffin, P. L., Rogers, K. L., Fogel, M. L., Hemley, R. J., & Steele, A. (2012). Extremophiles, 16(2), 355–361. doi:10.1007/s00792-011-0418-8

Effect of Network Polymerization on the Pressure-Induced Structural Changes in Sodium Aluminosilicate Glasses and Melts: 27 Al and 17 O Solid-State NMR Study

Lee, S. K., Yi, Y. S., Cody, G. D., Mibe, K., Fei, Y., & Mysen, B. O. (2012). The Journal of Physical Chemistry C, 116(3), 2183–2191. doi:10.1021/jp206765s

Novel Degenerate PCR Method for Whole-Genome Amplification Applied to Peru Margin (ODP Leg 201) Subsurface Samples

Martino, A. J., Rhodes, M. E., Biddle, J. F., Brandt, L. D., Tomsho, L. P., & House, C. H. (2012). Frontiers in Microbiology, 3(None), None. doi:10.3389/fmicb.2012.00017

Resolving phylogenetic signal from noise when divergence is rapid: A new look at the old problem of echinoderm class relationships

Pisani, D., Feuda, R., Peterson, K. J., & Smith, A. B. (2012). Molecular Phylogenetics and Evolution, 62(1), 27–34. doi:10.1016/j.ympev.2011.08.028

Early (Series 2) Cambrian archaeocyathan reefs of southern Labrador as a locus for skeletal carbonate production

Pruss, S. B., Clemente, H., & Laflamme, M. (2012). Lethaia, 45(3), 401–410. doi:10.1111/j.1502-3931.2011.00299.x

Photometric, spectral phase and temperature effects on 4 Vesta and HED meteorites: Implications for the Dawn mission

Reddy, V., Sanchez, J. A., Nathues, A., Moskovitz, N. A., Li, J-Y., Cloutis, E. A., … Archer, K. (2012). Icarus, 217(1), 153–168. doi:10.1016/j.icarus.2011.10.010

1...409/410/411/412/413...520