Abstract
High quality new data on the asteroid mass and volume were produced in the last years from both extra-atmospheric instruments and the groundbased high-performance telescopes. This paper presents a synthesis of these resultsin terms of the asteroid density, taking into account several techniques, and the possible correlation of the density through the taxonomic system. The important conclusion is that M-type asteroids seems to have an unexpected low density, which cannot be explained by the present mineralogy assumed by the comparative mineralogy.
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