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By - James Richardson et al, 2007
Summary - The Deep Impact produced a reasonably “well-behaved” oblique-impact cratering event. The resulting ejecta plume followed well-established scaling relationships for cratering in a medium-to-high porosity target material, consistent with a transient crater of not more than 85–140 m diameter, formed in not more than 250–550 s, for the case of Y = 0 Pa (gravity-dominated cratering), and not less than 22–26 m diameter, formed in not less than 1–3 s, for the case of Y = 10 kPa (strength-dominated cratering).
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Title - Deep Impact: Excavating Comet Tempel 1
By - A'Hearn et al, 2005
Summary -
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Title - The distribution of water ice in the interior of Comet Tempel 1
By - Jessica Sunshine et al, 2007
Summary -
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