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月球正面与背面的差异对比与演化分析
引用本文:姚美娟,陈建平,徐彬,籍进柱,陈剑.月球正面与背面的差异对比与演化分析[J].延边大学理工学报,2017,0(3):428-438.
作者姓名:姚美娟  陈建平  徐彬  籍进柱  陈剑
作者单位:1.中国地质大学(北京) 国土资源与高新技术研究中心,北京 100083; 2.中国地质大学(北京) 地球科学与资源学院,北京 100083; 3.中国科学院地球化学研究所 月球与行星科学研究中心,贵州 贵阳 550081;4.山东大学 空间科学研究院,山东 威海 264209
摘    要:月球的起源与演化以及月球正面与背面的差异性一直是科学研究的热点问题,月球正面和背面的差异性说明两个半球的演化过程存在不对称性。通过分析月球正面与背面的物理特征、岩石矿物特征和构造特征分布差异,研究形成月球正面和背面差异性的动力过程,进而解释月球正面与背面地质演化差异?结果表明:月球正面和背面的物理特征、岩石矿物特征和构造特征都存在很大的不同;月球正面和背面的地质演化可以划分为以内动力地质作用为主的阶段,内、外动力地质作用并存阶段和以外动力地质作用为主的阶段;以内动力地质作用为主的阶段和内、外动力地质作用并存阶段是造成月球正面和背面地质演化差异的两个主要阶段,而以外动力地质作用为主的阶段对月球正面和背面地质演化差异的形成影响较小。

关 键 词:月球  演化  正面  背面  物理特征  岩石矿物  构造特征

Difference Comparison and Evolution Analysis of Lunar Nearside and Farside
YAO Mei-juan,CHEN Jian-ping,XU Bin,JI Jin-zhu,CHEN Jian.Difference Comparison and Evolution Analysis of Lunar Nearside and Farside[J].Journal of Yanbian University (Natural Science),2017,0(3):428-438.
Authors:YAO Mei-juan  CHEN Jian-ping  XU Bin  JI Jin-zhu  CHEN Jian
Affiliation:1. Institute of High and New Techniques Applied to Land Resources, China University of Geosciences, Beijing 100083, China; 2. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 3. Center for Lunar and Planetary Sciences, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, Guizhou, China; 4. Institute of Space Sciences, Shandong University, Weihai 264209, Shandong, China
Abstract:The origin and evolution of Moon and the difference between lunar nearside and farside are hot topics. The difference between lunar nearside and farside shows the asymmetry evolution of the two hemispheres. Based on the analysis of the physical properties, rock mineral properties and structural characteristics of lunar nearside and farside, the difference of their geological evolution and the dynamic process of their formations were discussed. The results show that the physical properties, rock mineral properties and structural characteristics of lunar nearside and farside are different; the geological evolution history of Moon can be divided into three stages, including the stage of endogenic geological process, the stage of both endogenic and exogenic geological processes and the stage of exogenic geological process; the differences between lunar nearside and farside are mainly affected by the stage of endogenic geological process and the stage of both endogenic and exogenic geological processes, while the stage of exogenic geological process only takes little effect on lunar nearside and farside.
Keywords:Moon  evolution  nearside  farside  physical property  rock mineral  structural characteristic
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