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Exclusive: 'Super map’ rewrites moon’s geo-clock, ‘an important foundation for humanity to explore deep space,’ project scientists tell GT_我的网站

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A |             随着婴幼儿辅食从“满足基本喂养”迈向“精细化科学分阶”,如何将专业喂养理念更有效地传递给家庭,正成为行业与社会共同关注的话题。    

China's new geological map of the moon Photo: Courtesy of Institute of Geology under the Chinese Academy of Geological Sciences (CAGS)
    China's new geological map of the moon Photo: Courtesy of Institute of Geology under the Chinese Academy of Geological Sciences (CAGS)
A massive new geological map of the moon, measuring about 2.8 meters long and 1.2 meters high, has recently made its debut in China, offering one of the most comprehensive portraits yet of the lunar surface and its billions of years of geological evolution.
Compiled by the Institute of Geology under the Chinese Academy of Geological Sciences (CAGS), together with the Institute of Geochemistry under the Chinese Academy of Sciences, Jilin University, Shandong University and China University of Geosciences (Beijing), the 1:5,000,000-scale Geological Map of the moon marks 13,519 impact craters, 81 impact basins, 14 types of geological structures and 17 rock types, and includes detailed inset maps of the lunar north and south poles.
More than simply a new rendering of the lunar surface, the map incorporates the latest findings from China's Chang'e lunar exploration program. Scientists involved in the project told the Global Times in exclusive interviews that the new map recalibrates key boundaries in the moon's geological chronology, updates the distribution of important lunar rock types and establishes a more systematic framework for interpreting the moon's evolution.
"The Chang'e-5 and Chang'e-6 missions have successively returned samples from the moon's near and far side, producing findings that have significantly changed our understanding of lunar evolution," Ding Xiaozhong, a researcher at the Institute of Geology under CAGS and a core member of the mapping team, told the Global Times.
Samples showed that volcanic activity on the moon continued until about 2 billion years ago - roughly one billion years later than previously thought under the conventional framework. Meanwhile, observations and samples from the lunar far side have provided new information about the composition and magmatic history of the moon's deep interior, Ding said.
"These new discoveries created an urgent need for a new and systematic geological map that could integrate the latest data and research results and establish an updated framework for understanding lunar geology," he noted.
The 1:5,000,000 scale was chosen with practical applications in mind. Compared with China's more detailed 1:2,500,000 lunar geological atlas released in 2024, the new map provides a more condensed, global view of the Moon, enabling researchers to quickly identify major geological relationships while also making it suitable for education, popular science and the early-stage planning of exploration missions.
Jin Ming, an associate researcher at the Institute of Geology under CAGS, told the Global Times that the project also represents an important step toward establishing a mature Chinese standard for planetary geological mapping. Its newly designed symbols, legends and color system have been certified as a group standard by the Geological Society of China, filling a gap in China's standardized rules for planetary geological mapping.
Although the latest project formally began in 2022 and took about four years to complete, Ding and Jin said its scientific foundations stretch back decades. Data accumulation and methodology development began with China's early lunar exploration missions, particularly after Chang'e-1 started returning scientific data. Several generations of Chinese planetary geologists have since developed a comprehensive system for lunar geological interpretation, remote-sensing data processing and map compilation.
One of the toughest challenges was bringing together enormous quantities of remote-sensing data obtained by different instruments, Jin said. Different payloads aboard the Chang'e probes produced data with varying resolutions and spectral characteristics, requiring specially developed algorithms as well as extensive manual verification to place them under a unified mapping standard.
"We had to make the different datasets compatible under the same system while striking a balance between scientific completeness and visual clarity - avoiding information overload without losing critical geological clues," Jin said.
China previously released the world's first 1:2,500,000-scale high-precision lunar geological atlas in 2024. The newly completed 1:5,000,000 map is therefore not simply a reduced-scale copy, the scientists stressed, but a scientific update incorporating newly available data and revised interpretations of lunar chronology, lithology and geological evolution.
China's new lunar geological map has achieved an all-round improvement over previous versions and is now at the international forefront, Ding said. 
We are the only country to have exclusive access to directly measured sampling data from the Chang'e-5 and Chang'e-6 missions. By using age anchors from lunar samples independently obtained by China to calibrate the geological chronology, this new data source and calibration system represents a core advantage of China."
Like Earth, which is divided into geological periods such as the Cambrian and Jurassic, the Moon also has a geological timescale. One of the most significant tasks behind the new map was to recalibrate that "lunar clock."
According to Jin, the recalibration draws on two major sources - the latest international isotopic dating results, including updated measurements of Apollo samples and lunar meteorites, and the precise age obtained from Chang'e-5 samples.
The latter provided an especially important chronological anchor. Radiometric dating of Chang'e-5 basalt has placed its age at roughly 2 billion years, demonstrating that lunar volcanism persisted far later than had once been assumed and substantially changing scientists' picture of the moon's late-stage thermal evolution.
Based on the updated evidence, the team refined the starting ages of several ancient lunar periods, including the Aitkenian, Nectarian and Imbrian periods, to approximately 4.33 billion, 4.17 billion and 3.92 billion years ago, respectively.
More significantly, the researchers used the 2-billion-year age boundary to divide the Eratosthenian into an early and a late epoch. The team said this marks the first time an age boundary derived from samples independently collected by China has been incorporated into such a detailed Chinese lunar geological chronology.
"The moon's story itself has not changed, but its timeline has," Jin said. "We once thought that major lunar volcanism had essentially cooled down about 3 billion years ago. Now we know that the Moon remained volcanically active until at least about 2 billion years ago. That means the thermal evolution of the lunar interior and many of the causal relationships in its later history need to be re-examined."
Ding highlighted a newly mapped rock type in the South Pole-Aitken Basin - gabbronorite - identified with the help of the latest Chang'e-4 and Chang'e-6 exploration results. 
The vast basin on the lunar far side is one of the moon's largest and oldest impact crater.
"This is like being able to directly see material from deeper inside the moon," Ding said. "Previously, much of this could only be inferred from remote-sensing observations. With Chang'e-4 in-situ exploration and Chang'e-6's returned samples, we now have much stronger evidence for identifying its existence and distribution."
Another important revision concerns KREEP, a lunar geochemical component enriched in potassium, rare-earth elements and phosphorus and commonly associated with elevated concentrations of radioactive heat-producing elements such as thorium and uranium.
According to Ding, earlier models suggested that KREEP-rich material was concentrated in a relatively limited area. Higher-resolution data used in the new mapping project indicate a broader and more continuous distribution than previously thought, suggesting that its abundance may have been underestimated.
Ding said the finding is scientifically important not only for assessing potentially resource-rich lunar materials, but also because the distribution of KREEP provides clues to the crystallization of the early lunar magma ocean, the thickness of the lunar crust and the moon's internal thermal evolution.
The map's colors also carry geological meaning. The team follows a principle of "lighter for younger, darker for older": relatively young Copernican impact materials are depicted in bright pale yellow, ancient Aitkenian impact materials in deep purplish red, while mare basalts are represented in varying shades of blue.
"The color system combines the logic of geological evolution with elements of traditional Chinese color aesthetics, giving China's lunar geological maps a distinctive scientific and visual identity," Ding said.
Beyond basic science, the researchers said the new geological map can serve as a strategic base map for China's future lunar exploration, including subsequent Chang'e missions and planning related to the International Lunar Research Station (ILRS).
A refined geological chronology can help scientists understand the age and modification history of candidate regions; updated rock mapping can identify areas of particular scientific or resource interest; and the global-scale representation allows mission planners to compare broad regions before moving to higher-resolution site studies.
Asked whether the map could directly support the Chang'e-7 and Chang'e-8 missions, Jin stressed that its role is primarily strategic rather than tactical.
"The 1:5,000,000 geological map is a global-scale foundational map. It can be used for broad comparisons of potential landing regions and for evaluating their overall geological context," Jin said. "Precise landing-site selection and detailed rover-route planning, however, require higher-resolution regional geological maps. The two work together, moving progressively from the global scale to finer regional scales."
The scientists also stressed that the map is intended to be shared with the international scientific community. Digital versions are expected to be released through professional publications and public scientific databases, while the standardized symbols and mapping rules could facilitate exchanges with other planetary geological mapping systems.
Ding said significant room remains for international cooperation, from comparing and translating different geological mapping standards to joint studies of the evolution of the lunar far side and the origin of the ancient South Pole-Aitken Basin.
"China possesses unique exploration data and returned lunar samples, which provide a strong foundation for cooperation," Ding said, adding that planetary science, scientific training and deep-space exploration technologies all offer potential areas for expanded exchanges.
"A precise geological map of the moon is an important foundation for humanity to explore deep space and understand the universe," Jin said.
The latest map, he noted, is not an endpoint. As China proceeds with subsequent lunar exploration missions and acquires new observations and samples, the geological picture of the Moon will continue to be refined.
"Future exploration will allow us to keep updating our understanding of lunar geology," Jin said. "At the same time, we hope these results can contribute to broader international scientific cooperation and to humanity's exploration of the moon."
。2026年8月11日,英氏控股携手央视网正式上线公益短片《时代的托举》。短片以科学喂养知识普及为切口,聚焦中国宝宝辅食喂养方式的迭代升级,传递婴幼儿辅食“按阶段科学喂养”的理念,并以公益传播的方式助力更多家庭建立更规范、更健康的辅食喂养认知。守护生命早期营养!英氏控股携手央视网《时代的托举》诠释育儿时代进阶        时代之变:三代人的喂养变迁        《时代的托举》以三代人“爱的托举”为主线展开一个关于婴幼儿喂养的叙事:60年代那辈人把爱放在心尖,那时的喂养全凭经验,“让孩子吃饱”就是那个年代能给出的全部;90年代这辈人生活越过越好,追求营养充足、食材多样,“把最好的都给孩子”成了他们对爱的表达方式;如今,新一代家庭更关注科学喂养,他们关心的是每一口辅食是否精准匹配宝宝当下的发育阶段、是否经过了科学验证。       从凭经验到靠科学,记录中国三代人喂养观念的时代进阶,也致敬每一位为下一代成长默默托举的人。这正是时代变化的缩影。

B | 守护生命早期营养!英氏控股携手央视网《时代的托举》诠释育儿时代进阶        科学之路:让喂养有标准可依        短片将个体家庭的喂养选择与宏观政策演进相呼应,《国民营养计划》将“生命早期1000天营养健康行动”写入国家文件、中国营养学会启动婴幼儿辅食科学分阶喂养标准化建设这些被融入故事中,让观众看到科学喂养如何从一个家庭的日常选择,上升为一个国家对下一代最长远的承诺。短片同时记录了中国辅食行业从零起步、用不到四十年走过了别人一百多年路的奋斗历程,最终落脚于一个朴素而有力的判断:喂养的方式在变,但三代人向上托举的方向从未改变——今天的“科学喂养”,正是这份托举在新时代的延续。       作为品牌全面升级后的重要一步,英氏控股联合央视网打造《时代的托举》,为辅食行业共同发声:科学辅食筑基石,强健民族新一代。央视网是中央广播电视总台主办的中央重点新闻网站和国家级互联网视频综合传播服务平台,央视网的深度参与,不仅源于其在国家级媒体平台的内容制作与传播优势,更在于这个议题本身的分量——当“生命早期1000天”被写入国家文件、“科学喂养”便不再只是个体家庭的选择,而是关乎国民健康根基的公共议题。

C | 这正是值得被国家级媒体记录和传播的时代命题。此次《时代的托举》从脚本打磨到视觉呈现,央视网深度参与内容共创与视频制作,以专业的内容把控能力和广阔的社会洞察视角,将科学喂养的时代命题转化为打动人心的影像语言,将科学喂养这一民生话题提升至国家叙事高度,为短片的传播提供了坚实的品质保障与公信力支撑。       当科学成为新时代的育儿答案,行业也正在寻找共同语言。2026年5月,中国营养学会正式发布《婴幼儿辅食质地五阶分级指南》团体标准,英氏控股作为核心起草单位之一深度参与共建。标准发布后,英氏控股第一时间完成“科学5阶喂养体系”及全线产品的全面升级,从包装显性化到产品标准化,率先将团体标准确立的科学分阶依据转化为消费者可感知的产品事实。此次携手央视网推出《时代的托举》,则是英氏控股在完成品牌升级后,面向社会大众的一次价值传递:将“科学辅食”从行业标准推向公共认知,让科学喂养理念走进千家万户。守护生命早期营养!英氏控股携手央视网《时代的托举》诠释育儿时代进阶        品牌之责:科学喂养守护下一代成长        从一勺米粉到一个行业的科学标准,从一个品牌的18年深耕到一个国家对下一代的长远承诺,《时代的托举》所讲述的,是一份跨越代际的责任与担当。从参与标准共建到率先落地标准实践,再到推出核心宣传片,英氏控股所践行的,是“科学辅食筑基石,强健民族新一代”的核心。       作为中国婴幼儿辅食第一品牌,英氏控股深知市场份额的背后是责任,行业地位的背后是担当。在产品层面,英氏控股有责任引领产品技术迭代,为中国宝宝带来更高品质的辅食产品;在行业标准层面,英氏控股有责任推动整个行业从“概念混战”走向“标准规范”,让科学喂养成为行业共识而非个别企业的孤军奋战;在消费者教育层面,英氏控股有责任将“辅食科学喂养”理念普及到每一个中国家庭。       《时代的托举》并不只是在讲述一支公益短片的上线,它更像是一次面向社会的集体回望:回望中国家庭如何一步步从经验喂养走向科学喂养,也回望英氏控股如何从企业成长为行业标准建设的重要参与者。站在“健康中国”的新起点上,英氏控股将继续以科学为底座、以责任为引擎,与央视网以及更多权威力量一道,把“科学喂养”这件关乎千家万户的事,做得更深入、更扎实,也更长久。

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