Geology and tectonics of Beta Regio, Guinevere Planitia, Sedna Planitia, and Western Eistla Regio, Venus: Results from Arecibo image data
D. A. Senske(Jet Propulsion Laboratory), J. K. Harmon(University of Puerto Rico at Arecibo), J. C. Aubele, J. W. Head(John Brown University), D. B. Campbell(Cornell University), P. C. Fisher(Brown University), E. R. Stofan(Smithsonian Institution), N.J.S. Stacy(Defence Science and Technology Group), A. A. Hine(University of Puerto Rico at Arecibo)
Cited by 11
Related Papers
Character and Spatial Distribution of OH/H <sub>2</sub> O on the Surface of the Moon Seen by M <sup>3</sup> on Chandrayaan-1
|Science|2009|842
Recent ice ages on Mars
|Nature|2003|780
Ascent and eruption of basaltic magma on the Earth and Moon
|Journal of Geophysical Research Atmospheres|1981|726
Geologic history of Mars
|Earth and Planetary Science Letters|2009|694
Evidence for a subsurface ocean on Europa
|Nature|1998|585