Book contents
- Remote Compositional Analysis
- Cambridge Planetary Science
- Remote Compositional Analysis
- Copyright page
- Contents
- Contributors
- Foreword
- Preface
- Acknowledgments
- Part I Theory of Remote Compositional Analysis Techniques and Laboratory Measurements
- Part II Terrestrial Field and Airborne Applications
- Part III Analysis Methods
- Part IV Applications to Planetary Surfaces
- 17 Spectral Analyses of Mercury
- 18 Compositional Analysis of the Moon in the Visible and Near-Infrared Regions
- 19 Spectral Analyses of Asteroids
- 20 Visible and Near-Infrared Spectral Analyses of Asteroids and Comets from Dawn and Rosetta
- 21 Spectral Analyses of Saturn’s Moons Using the Cassini Visual Infrared Mapping Spectrometer
- 22 Spectroscopy of Pluto and Its Satellites
- 23 Visible to Short-Wave Infrared Spectral Analyses of Mars from Orbit Using CRISM and OMEGA
- 24 Thermal Infrared Spectral Analyses of Mars from Orbit Using the Thermal Emission Spectrometer and Thermal Emission Imaging System
- 25 Thermal Infrared Remote Sensing of Mars from Rovers Using the Miniature Thermal Emission Spectrometer
- 26 Compositional and Mineralogic Analyses of Mars Using Multispectral Imaging on the Mars Exploration Rover, Phoenix, and Mars Science Laboratory Missions
- 27 Mössbauer Spectroscopy at Gusev Crater and Meridiani Planum
- 28 Elemental Analyses of Mars from Rovers Using the Alpha-Particle X-Ray Spectrometer
- 29 Elemental Analyses of Mars from Rovers with Laser-Induced Breakdown Spectroscopy by ChemCam and SuperCam
- 30 Neutron, Gamma-Ray, and X-Ray Spectroscopy of Planetary Bodies
- 31 Radar Remote Sensing of Planetary Bodies
- Index
- References
20 - Visible and Near-Infrared Spectral Analyses of Asteroids and Comets from Dawn and Rosetta
from Part IV - Applications to Planetary Surfaces
Published online by Cambridge University Press: 15 November 2019
- Remote Compositional Analysis
- Cambridge Planetary Science
- Remote Compositional Analysis
- Copyright page
- Contents
- Contributors
- Foreword
- Preface
- Acknowledgments
- Part I Theory of Remote Compositional Analysis Techniques and Laboratory Measurements
- Part II Terrestrial Field and Airborne Applications
- Part III Analysis Methods
- Part IV Applications to Planetary Surfaces
- 17 Spectral Analyses of Mercury
- 18 Compositional Analysis of the Moon in the Visible and Near-Infrared Regions
- 19 Spectral Analyses of Asteroids
- 20 Visible and Near-Infrared Spectral Analyses of Asteroids and Comets from Dawn and Rosetta
- 21 Spectral Analyses of Saturn’s Moons Using the Cassini Visual Infrared Mapping Spectrometer
- 22 Spectroscopy of Pluto and Its Satellites
- 23 Visible to Short-Wave Infrared Spectral Analyses of Mars from Orbit Using CRISM and OMEGA
- 24 Thermal Infrared Spectral Analyses of Mars from Orbit Using the Thermal Emission Spectrometer and Thermal Emission Imaging System
- 25 Thermal Infrared Remote Sensing of Mars from Rovers Using the Miniature Thermal Emission Spectrometer
- 26 Compositional and Mineralogic Analyses of Mars Using Multispectral Imaging on the Mars Exploration Rover, Phoenix, and Mars Science Laboratory Missions
- 27 Mössbauer Spectroscopy at Gusev Crater and Meridiani Planum
- 28 Elemental Analyses of Mars from Rovers Using the Alpha-Particle X-Ray Spectrometer
- 29 Elemental Analyses of Mars from Rovers with Laser-Induced Breakdown Spectroscopy by ChemCam and SuperCam
- 30 Neutron, Gamma-Ray, and X-Ray Spectroscopy of Planetary Bodies
- 31 Radar Remote Sensing of Planetary Bodies
- Index
- References
Summary
New visible and infrared data of minor bodies, including minor planet 1 Ceres, asteroids 4 Vesta, 21 Lutetia, 2867 Steins and comet 67P/Churyumov–Gerasimenko (hereafter 67P/CG) have been collected in the last years by remote sensing instruments aboard NASA-Dawn and ESA-Rosetta missions. These minor bodies are among the most primitive bodies in the Solar System, and the understanding of their composition, surface morphology and evolution history is a fundamental step to shed light on the processes that occurred during planetary formation.By merging spatial and spectral information retrieved from the surfaces of these objects it is possible to infer their composition and physical properties and to correlate them with local morphology and geological processes. A discussion about spectral indicators, modeling, and mapping is given for both asteroids and comet 67P/CG. Given that the remote sensing observation techniques are very similar between Dawn and Rosetta missions, a comparative approach is used for the entire chapter and methods and interpretation for the results of these different objects are given together.
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- Remote Compositional AnalysisTechniques for Understanding Spectroscopy, Mineralogy, and Geochemistry of Planetary Surfaces, pp. 413 - 427Publisher: Cambridge University PressPrint publication year: 2019