Amorphous and crystalline ice on the Galilean satellites: A balance between thermal and radiolytic processes
By G. Hansen, T. McCord. 2003
176 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/a670765533fd8f471dad7eb27fcd8ae182d5ef8d
How researchers see this paper
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In Astronomy and Astrophysics
- François Poulet
- Dale P. Cruikshank
- J. Carter
- M. Bernstein
- Ted L. Roush
- S. Sandford
- R. Mastrapa
- Cristina Dalle Ore
In Atmospheric Science
- Dale P. Cruikshank
- J. Carter
- Ted L. Roush
- S. Sandford
- R. Mastrapa
- Cristina Dalle Ore
- T. Bartels-Rausch
Citations in the corpus
- OPTICAL CONSTANTS OF AMORPHOUS AND CRYSTALLINE H2O-ICE: 2.5–22 μm (4000–455 cm−1) OPTICAL CONSTANTS OF H2O-ICE (2009, methodology): “Hansen & McCord (2004) examined this region in NIMS data to assess the distribution of amorphous and crystalline H2O-ice on Ganymede.”
- Optical constants of amorphous and crystalline H2O-ice in the near infrared from 1.1 to 2.6 μm (2008, background): “However, the detection of amorphous H2O-ice on the surface of Europa (Hansen and McCord, 2004) indicates that amorphization occurs on a surface where the temperature ranges from 100 to 150 K (Spencer et al., 1999).”
- VLT/SINFONI OBSERVATIONS OF EUROPA: NEW INSIGHTS INTO THE SURFACE COMPOSITION (2016, background): “According to a study based on the 3.1 μm water absorption, H2O ice on Europa is presumed to be mainly amorphous (Hansen & McCord 2004).”