首页|A lunar time scale from the perspective of the Moon's dynamic evolution

A lunar time scale from the perspective of the Moon's dynamic evolution

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A geologic time scale is a chronological system that separates the geological strata of a planetary body into different units in temporal sequence and shows its progressive evolution.The time scale of the Moon was established a half-century ago during the telescopic-early Apollo exploration era,using data with limited spatial coverage and resolution.The past decades have seen a wide array of studies,which have significantly extended our understanding of global lunar geologic evolution.Based on a comprehensive review of lunar evolution with respect to the dynamical changes,we propose two major updates to the current lunar time scale paradigm to include the evolution of both endogenic and exogenic dynamic forces now known to have influenced early lunar history.Firstly,based on the temporal interplay of exogenic and endogenic processes in altering the Moon,we defined three Eon/Eonothem-level units to represent three dynamical evolutionary phases.Secondly,the pre-Nectarian System is redefined and divided as the magma ocean-era Magma-oceanian System and the following Aitkenian System beginning with the South Pole-Aitken basin.The ejecta of this basin,Das Formation,was deposited on the primordial lunar crust as the oldest stratum produced from exogenic processes.The updated lunar time scale,facilitated by the post-Apollo exploration and research advances,provides an integrated framework to depict the evolution of the Moon and has important implications for the geologic study of other terrestrial planets.

The MoonGeologic time scaleEvolution historyEndogenic processExogenic process

Dijun GUO、Jianzhong LIU、James W.HEAD、Fuqin ZHANG、Zongcheng LING、Shengbo CHEN、Jianping CHEN、Xiaozhong DING、Jinzhu JI、Ziyuan OUYANG

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State Key Laboratory of Space Weather,National Space Science Center,Chinese Academy of Sciences,Beijing 100190,China

Center for Lunar and Planetary Sciences,Institute of Geochemistry,Chinese Academy of Sciences,Guiyang 550081,China

Center for Excellence in Comparative Planetology,Chinese Academy of Sciences,Hefei 230026,China

Department of Earth,Environmental and Planetary Sciences,Brown University,Providence RI02912,USA

Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China

Shandong Provincial Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment,Institute of Space Sciences,Shandong University,Weihai 264209,China

College of Geoexploration Science and Technology,Jilin University,Changchun 130026,China

School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China

Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China

School of Resources and Environmental Engineering,Inner Mongolia University of Technology Hohhot 010051,China

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National Key Research and Development Program of ChinaB-type Strategic Priority Program of the Chinese Academy of SciencesNational Natural Science Foundation of ChinaNational Natural Science Foundation of ChinaNational Natural Science Foundation of ChinaNational Science and Technology Infrastructure Work Projects

2022YFF0503100XDB410000004190231741941002417730652015FY210500

2024

中国科学:地球科学(英文版)
中国科学院

中国科学:地球科学(英文版)

影响因子:1.002
ISSN:1674-7313
年,卷(期):2024.67(1)
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