Seamless maps of major elements of the Moon: Results from high-resolution geostationary satellite

被引:0
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作者
Yu Lu [1 ,2 ,3 ]
Yun-Zhao Wu [1 ,4 ]
Cui Li [1 ]
Jin-Song Ma [5 ,6 ]
Wen-Wen Qi [7 ]
Wei Tan [7 ]
Xiao-Man Li [7 ]
Zhi-Cheng Shi [7 ]
Hong-Yan He [7 ]
Shu-Wu Dai [8 ]
Guo Li [8 ]
Feng-Jing Liu [8 ]
Jing-Qiao Wang [9 ]
Xiao-Yan Wang [9 ]
Qi Wang [10 ]
Ling-Jie Meng [10 ]
机构
[1] Earth Observation System and Data Center, China National Space Administration
[2] Key Laboratory of Planetary Sciences, Purple Mountain Observatory, Chinese Academy of Sciences
[3] School of Astronomy and Space Science, University of Science and Technology of China
[4] CAS Center for Excellence in Comparative Planetology
[5] Space Science Institute, Macau University of Science and Technology
[6] School of Geography and Ocean Science, Nanjing University
[7] Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application
[8] Beijing Institute of Space Mechanics and Electricity
[9] Beijing Institute of Spacecraft System Engineering
[10] China Centre for Resources Satellite Data and Application
基金
中国国家自然科学基金; 国家重点研发计划;
关键词
D O I
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中图分类号
P184 [月球];
学科分类号
070401 ;
摘要
Major elements such as Fe, Ti, Mg, Al, Ca and Si play very important roles in understanding the origin and evolution of the Moon. Previous maps of these major elements derived from orbital data are based on mosaic images or low-resolution gamma-ray data. The hue variations and gaps among orbital boundaries in the mosaic images are not conducive to geological studies. This paper aims to produce seamless and homogenous distribution maps of major elements using the single-exposure image of the whole lunar disk obtained by China’s high-resolution geostationary satellite, Gaofen-4, with a spatial resolution of~500 m. The elemental contents of soil samples returned by Apollo and Luna missions are regarded as ground truth, and are correlated with the reflectance of the sampling sites extracted from Gaofen-4 data.The final distribution maps of these major oxides are generated with the statistical regression model. With these products, the average contents and proportions of the major elements for maria and highlands were estimated and compared. The results showed that Si O2and Ti O2have the highest and lowest fractions in mare and highland areas, respectively. Moreover, the relative concentrations of these elements could serve as indicators of geologic processes, e.g., the obviously asymmetric distributions of Al2O3, Ca O and Si O2around Tycho crater may suggest that Tycho crater was formed by an oblique impact from the southwest direction.
引用
收藏
页码:54 / 62
页数:9
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