1：250万月球酒海幅（LQ-20）地质图编研

刘敬稳; 刘建忠; 朱凯; 张敬宜; 张珂; 吴聪哲; 雷丹泓

doi:10.11834/jrs.20243512

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1：250万月球酒海幅（LQ-20）地质图编研
1：250，000 Geological Map Compilation and Research of the Nectaris Quadrangle （LQ-20） on the Moon
2024年页码：1-13
网络出版日期： 2024-04-02 ，
DOI： 10.11834/jrs.20243512

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刘敬稳，刘建忠，朱凯，张敬宜，张珂，吴聪哲，雷丹泓.XXXX.1：250万月球酒海幅（LQ-20）地质图编研.遥感学报，XX（XX）： 1-13

LIU Jingwen，LIU Jianzhong，ZHU Kai，ZHANG Jingyii，ZHANG Ke，WU Congzhei，LEI Danhong. XXXX. 1：250，000 Geological Map Compilation and Research of the Nectaris Quadrangle （LQ-20） on the Moon. National Remote Sensing Bulletin， XX（XX）：1-13
刘敬稳，刘建忠，朱凯，张敬宜，张珂，吴聪哲，雷丹泓.XXXX.1：250万月球酒海幅（LQ-20）地质图编研.遥感学报，XX（XX）： 1-13 DOI： 10.11834/jrs.20243512.

LIU Jingwen，LIU Jianzhong，ZHU Kai，ZHANG Jingyii，ZHANG Ke，WU Congzhei，LEI Danhong. XXXX. 1：250，000 Geological Map Compilation and Research of the Nectaris Quadrangle （LQ-20） on the Moon. National Remote Sensing Bulletin， XX（XX）：1-13 DOI： 10.11834/jrs.20243512.

摘要

在嫦娥探月数据及其他月球地质资料的基础上，中国科学院地球化学研究所主导的团队编制了比例尺为1：250万的全月地质图、月球分幅地质图、月球构造纲要图、月球岩石分布图以及30分幅地质图，其中就包括LQ-20酒海幅。LQ-20图幅以其独特的酒海纪与艾肯纪交界的标志事件——酒海盆地撞击事件而引人注目。本文详细介绍了月球地质图的编研的发展历史、LQ-20分幅图的图幅表达的内容，并阐述了该图幅表达的岩石类型、撞击盆地和撞击坑物质、构造形迹特征等：图幅中表达了12类岩石类型、8个盆地的地质信息、260个撞击坑的坑物质、16类构造形迹特征，涉及了整个三宙六纪的地质信息。最后讨论了该月球图幅区域内从岩浆洋纪到哥白尼纪的整体区域地质演化历史、并通过对比分析LQ20的制图结果提出我国1：250万月球地质图与美国月球地质图在表达地质信息上的本质区别在于其对月球地质过程整体的地质体系的完整建立与系统表达，每处地质信息都明确表达其地质作用来源，每个区域都有层次分明的按形成顺序排列的地质过程，这充分论证了我国1：250万月球地质图能够为我国乃至全球月球就位探测、科学研究等提供了一份详尽的月球地质背景资料。

Abstract

Based on the Chang'E lunar exploration data and other lunar geological data

the team led by the Institute of Geochemistry of the Chinese Academy of Sciences has compiled a series of lunar global geological maps. These maps include a 1:2

500

000-scale global geologic map

a digital global lithologic map

and a global tectonic map. At the same time

30 lunar quadrangle geological maps were also compiled

including the LQ-20 Nectaris Quadrangle map. The LQ-20 map is eye-catching because it depicts the impact event of the Mare Nectaris Basin

which divided the Nectarian and Aitkenian periods

during the Nectarium classic formation event.This article provides a detailed overview of the development history of lunar geological mapping. It discusses the various geological features observed in the LQ-20

including rock types

impact basins

crater materials

and structural characteristics：12 rock types

basin formations on 8 impact basins

crater materials from 260 impact craters

and 16 types of structural characteristics

which covering geological information in the sixth periods.Finally

we discussed the regional geological evolution history of the LQ-20 map from the Magmatic Oceanic Period to the Copernican Period. We also compared the expression of geological features in the LQ-20 map to that of the USGS lunar geological map

highlighting the differences and advantages: the fundamental distinction in conveying geological information lies in the comprehensive establishment and systematic representation of the overall lunar geological processes as an integrated geological system; this involves providing a clear explanation of the geological causes for each unit

ensuring that each geological feature conveys its origin; furthermore

each region is characterized by a distinct hierarchy of geological units arranged in chronological order. This project would provide lunar geological background information for lunar exploration

scientific research

and related endeavors

benefiting not only China but also the global communities.

关键词

月球地质图LQ-20酒海盆地遥感解译月球地质演化历史

Keywords

lunar geological mapLQ-20Mare NectarisRemote Sensing InterpretationGeological Evolution History

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