Except for the major basins (e.g., Orientale, Schrödinger, Imbrium, Crisium, Apollo, and Nectaris Basin), detailed sub-formation interpretations for most other basins are lacking, which hampers the construction of a complete (global) geological interpretation for the lunar impact basins. Due to the different identification standards currently used, the basin identification results are highly inconsistent. Impact basins are primary geological structures on the Moon, and play key roles in revealing the lunar history. This method is a typical application of lunar big-data-driven knowledge discovery and will help promote the transformation of lunar landing area selection from traditional qualitative analyses to automated intelligence optimization. The results at different resolutions are relatively stable and are consistent with the distribution of craters or basins in the lunar mantle and the spatial distribution of olivine, which proves the effectiveness and feasibility of this method. Among them, the first gradient is 58% and 58.7%, and the second gradient is 26% and 23.9%. When comparing and analyzing the posterior probability map of the landing zones with the known landing points and the artificially preferred landing zones, it is found that 84% and 82.6% fall within the suitable landing zones, respectively. The result of the weights of evidence is further constrained by the complexity of the number of cells and the complexity of the distribution, and the posterior probability map of suitable landings is finally obtained. The distribution complexity of impact craters in each cell is calculated according to the fractal. According to the semi-parabolic distribution in the fuzzy distribution, the fuzzy membership degree of the impact crater radius is presented and the complexity of the number of impact craters in a cell is calculated. After all moon data are divided into grids, the prior probability of each evidence factor, the in-cell weight of each evidence factor, and the Bayesian posterior probability are calculated. The method takes the thickness of the lunar crust, roughness, slope, digital elevation model, gravity gradient, iron oxide distribution, and lunar soil optical maturity as evidence layers, and known landing sites as the target layer. This paper proposes a new method that strategically applies the weights of evidence (WoE) and fractals to optimize the landing area of the detector in the whole moon. Factors such as engineering constraints, scientific goals, and resource requirements are comprehensively considered. Under the premise that big data, artificial intelligence, and other technologies are becoming increasingly mature, with in-depth analysis and the mining of lunar-related digital data, it is possible to automatically optimize the landing zones in the whole moon. Generally, it is artificially limited to a small zone, and there are few effective quantitative models for landing areas. So you can see where geological features like craters and plateaus are located and when they formed.At present, the selection of lunar landing areas is mostly determined by experts’ argumentation and experience. With bright colors, the map charts the moon's surface features and time periods. Using new and old data, the researchers created unified descriptions of the moon's rock layers. Scientists created the 1:5,000,000-scale geologic map using information from recent satellite trips to the moon and six regional maps from the Apollo era. In other words, you can check out the same blueprint that'll help NASA plan for future missions to the moon. #MOON ATLAS ONLINE PROFESSIONAL#But it's not just for professional scientists: The digital map is available online so people outside the scientific community can explore the moon's surface. In collaboration with NASA and the Lunar Planetary Institute, scientists from the USGS Astrogeology Science Center created the “Unified Geologic Map of the Moon.” The definitive blueprint of the lunar surface, it will serve as an invaluable reference for future human missions to the moon and additional lunar science. Have you ever looked up at the moon lighting up the night sky and wanted to know about its cratered surface? Well, now you can take a closer look at its geology because The United States Geological Survey (USGS) just released the most comprehensive geological map of the moon ever created.įor the first time ever, scientists have mapped out the entire surface of the moon.
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