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Hydrothermal fluid activity on asteroid Itokawa - Nature Astronomy

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Hydrothermal fluid activity on asteroid Itokawa - Nature Astronomy

Carbonaceous chondrites contain widespread mineralogical evidence for water–rock interactions, indicating that the C-type asteroids from which they are derived had active hydrothermal systems. In comparison, ordinary chondrites contain secondary minerals that are predominantly anhydrous, suggesting that their parent S-type asteroids were relatively dry. The returned particles from the Hayabusa Mission allow us to probe directly the alteration history of S-type asteroid Itokawa.

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Hydrothermal fluid activity on asteroid Itokawa - Nature Astronomy

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Hydrothermal fluid activity on asteroid Itokawa - Nature Astronomy

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