Binder A B
Lunar Research Institute, 1180 Sunrise Drive, Gilroy, CA 95020, USA.
Science. 1998 Sep 4;281(5382):1475-6. doi: 10.1126/science.281.5382.1475.
Lunar Prospector is providing a global map of the composition of the moon and analyzing the moon's gravity and magnetic fields. It has been in a polar orbit around the moon since 16 January 1998. Neutron flux data show that there is abundant H, and hence probably abundant water ice, in the lunar polar regions. Gamma-ray and neutron data reveal the distribution of Fe, Ti, and other major and trace elements on the moon. The data delineate the global distributions of a key trace element-rich component of lunar materials called KREEP and of the major rock types. Magnetic mapping shows that the lunar magnetic fields are strong antipodal to Mare Imbrium and Mare Serenitatis and has discovered the smallest known magnetosphere, magnetosheath, and bow shock complex in the solar system. Gravity mapping has delineated seven new gravity anomalies and shown that the moon has a small Fe-rich core of about 300 km radius.
“月球勘探者号”正在绘制月球成分的全球地图,并分析月球的重力场和磁场。自1998年1月16日以来,它一直在绕月极地轨道运行。中子通量数据显示,月球极地地区存在大量的氢,因此很可能存在大量的水冰。伽马射线和中子数据揭示了月球上铁、钛以及其他主要和微量元素的分布情况。这些数据描绘了月球物质中一种富含关键微量元素的成分——克里普岩以及主要岩石类型的全球分布。磁场测绘表明,月球磁场在雨海和澄海的对映点处很强,并发现了太阳系中已知最小的磁层、磁鞘和弓形激波复合体。重力测绘描绘出了七个新的重力异常区域,并表明月球有一个半径约300公里的富含铁的小核心。