Southwest Research Institute and NASA Solar System Exploration Research Virtual Institute (SSERVI)-Institute for the Science of Exploration Targets (ISET), Boulder, CO, USA.
Institute of Astronomy, Charles University, V Holešovičkách 2, CZ-18000, Prague 8, Czech Republic.
Science. 2015 Apr 17;348(6232):321-3. doi: 10.1126/science.aaa0602.
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.
内太阳系已知的最大和最近的碰撞事件是月球形成的大碰撞,即一个大型原行星和原地球之间的碰撞。它不仅在地球附近形成了一个圆盘,从而形成了月球,还将地球质量的百分之几抛出了地月系统。在这里,我们认为,那次事件中的许多千米大小的喷射碎片以超过 10 公里/秒的速度撞击了主带小行星,足以加热和除去目标岩石的气体。与通常以 5 公里/秒的速度发生的主带碰撞相比,这种撞击会产生数量级多 1000 倍的高热材料。通过对其时间演化进行建模,并将结果拟合到石质陨石中的古老撞击加热特征,我们推断月球形成于约 44.7 亿年前,这与之前的估计相符。