地史早期古板块构造研究进展  

RESEARCH PROGRESS OF PALAEO-PLATE TECTONICS IN THE EARLY GEOLOGICAL HISTORY

作　　者：袁建平[1] 倪志耀[2] 毕华[1] 

机构地区：[1]海南师范学院资源环境与旅游系,海南海口571158 [2]成都理工大学地球科学学院,四川成都610059

出　　处：《矿物岩石》2003年第1期46-50,共5页Mineralogy and Petrology

摘　　要：系统地总结早前寒武纪地质研究成果中与板块构造相关的一些线索以及对在地史早期寻找古板块的不利因素 ;在与现代洋壳结构对比的基础上 ,描述了地史早期洋壳残片的特征 ,为在现代大陆中寻找古板块提供了依据 ,并例证现今至少已经找到了早元古时期的洋壳残片。The research achievement on the early Precambrian in association with plate tectonics has been reviewed and summarized.Unfavourable factors concerning with the discovery of palaeoplates have been listed.In comparision of the ancient oceanic crustal structure with the modern one,the characteristics of oceanic slices in the early geological history have been described and evidence has been provided for seeking the palaeoplates in the modern continents.

关 键 词：板块构造 洋壳残片 地史早期 

分 类 号：P542.4[天文地球—构造地质学]