An Archaean heavy bombardment from a destabilized extension of the asteroid belt
William F. Bottke (),
David Vokrouhlický,
David Minton,
David Nesvorný,
Alessandro Morbidelli,
Ramon Brasser,
Bruce Simonson and
Harold F. Levison
Additional contact information
William F. Bottke: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
David Vokrouhlický: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
David Minton: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
David Nesvorný: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
Alessandro Morbidelli: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
Ramon Brasser: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
Bruce Simonson: Oberlin College
Harold F. Levison: Southwest Research Institute and NASA Lunar Science Institute, 1050 Walnut Street, Suite 300, Boulder, Colorado 80302, USA
Nature, 2012, vol. 485, issue 7396, 78-81
Abstract:
The Late Heavy Bombardment lasted much longer than previously thought, up to 1.7 billion years ago on Earth, with impacts on the Moon and Earth coming mostly from the E-belt-survivor Hungaria asteroids.
Date: 2012
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DOI: 10.1038/nature10967
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