基于嫦娥数据澄海—静海幅地质图编研  

The lunar geological mapping based on Chang'e data:Serenitatis-Tranquillitatis area as an example

作　　者：陈建平[1,2] 王翔[1,3] 王楠[1,2] 李婧[1,2] 姚美娟[1,2] 李洪克 

机构地区：[1]中国地质大学(北京),北京100083 [2]中国地质大学(北京)国土资源与高新技术研究中心,北京100083 [3]中国地质调查局发展研究中心,北京100037

出　　处：《地学前缘》2014年第6期7-18,共12页Earth Science Frontiers

基　　金：国家自然科学基金项目(41373068)

摘　　要：月球地质图(The Geological Map of the Moon),又称月面地质图、月面地质分区图,表示月球表面不同时代、不同类型的物质分布特征的平面图。月球地图和地图集编制工作是月球探测和科学研究的最重要内容之一。通过充分剖析50年前最早月球地质图与近期完成的虹湾幅、哥白尼幅地质图,采用嫦娥一期、二期CCD数据,配合数字高程、IIM以及LRO数据,文中以澄海—静海幅为研究区域,完成以地质背景、构造类型、地层时代、物质单元、盆地建造、火山碎屑分布、玄武岩厚度为主体要素的中国第一幅澄海—静海幅月球地质图编制,并且系统制定月球地质编图整个系统工程的设计方案,结合国内数字地质编图的技术标准和规范,建立中国自己的月球与行星地质编图标准、规范和制图流程。相关编图经验可以推广到火星地质图和金星地质图奠定技术基础。The geological map of the moon,also known as the geological map of the lunar surface or the lunar surface geological zoning map,shows the characteristics of the distribution of different kinds of matter in the lunar surface in different periods.Mapping the lunar maps and atlases is one of the most important works of lunar exploration and scientific research.Through full analysis of the first lunar geological map finished 50 years ago and the recently completed Sinus Tridum,Copernicus geological map,and using Chang＇e I,II CCD data,and digital elevation,IIM and LRO data,we selected Serenitatis-Tranquillitatis area as the study area and completed the first Serenitatis-Tranquillitatis area lunar geological map,in which the geological background,structure type,stratigraphic age,material unit,basin structure,pyroclastic distribution,and basalt thickness are the main elements.We developed a systematic mapping engineering plan,combined with domestic technical standards and specifications of digital geological mapping and established our own lunar and planetary geological mapping standards,specifications and mapping processes.The experience can be extended to geological mapping of Mars and Venus as the technical foundation.

关 键 词：地质图 澄海—静海 嫦娥 虹湾 

分 类 号：P184.62[天文地球—天文学]