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| Content Provider | World Health Organization (WHO)-Global Index Medicus |
|---|---|
| Author | Bottke, W. F. Scott, E. R. D. Weirich, J. R. Swindle, T. Vokrouhlický, D. Marchi, S. Levison, H. |
| Description | Author Affiliation: Bottke WF ( Southwest Research Institute and NASA Solar System Exploration Research Virtual Institute (SSERVI)-Institute for the Science of Exploration Targets (ISET), Boulder, CO, USA. bottke@boulder.swri.edu.); Vokrouhlický D ( Institute of Astronomy, Charles University, V Holesovickách 2, CZ-18000, Prague 8, Czech Republic.); Marchi S ( Southwest Research Institute and NASA Solar System Exploration Research Virtual Institute (SSERVI)-Institute for the Science of Exploration Targets (ISET), Boulder, CO, USA.); Swindle T ( Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ, USA. SSERVI Center for Lunar Science Exploration, Houston, TX, USA.); Scott ER ( Hawai'i Institute of Geophysics and Planetology, University of Hawai'i at Manoa, Honolulu, Hawai'i 96822, USA.); Weirich JR ( Department of Earth Sciences, Western University, London, ON, Canada.); Levison H ( Southwest Research Institute and NASA Solar System Exploration Research Virtual Institute (SSERVI)-Institute for the Science of Exploration Targets (ISET), Boulder, CO, USA.) |
| Abstract | The inner solar system's biggest and most recent known collision was the Moon-forming giant impact between a large protoplanet and proto-Earth. Not only did it create a disk near Earth that formed the Moon, it also ejected several percent of an Earth mass out of the Earth-Moon system. Here, we argue that numerous kilometer-sized ejecta fragments from that event struck main-belt asteroids at velocities exceeding 10 kilometers per second, enough to heat and degas target rock. Such impacts produce ~1000 times more highly heated material by volume than do typical main belt collisions at ~5 kilometers per second. By modeling their temporal evolution, and fitting the results to ancient impact heating signatures in stony meteorites, we infer that the Moon formed ~4.47 billion years ago, which is in agreement with previous estimates. |
| ISSN | 00368075 |
| Issue Number | 6232 |
| Journal | Science |
| Volume Number | 348 |
| e-ISSN | 10959203 |
| Language | English |
| Publisher | American Association for the Advancement of Science (United States) |
| Publisher Date | 2015-04-17 |
| Publisher Place | United States |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Multidisciplinary |
| Content Type | Text |
| Resource Type | Article |
| Subject | History and Philosophy of Science |
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