摘要
通过区域地球物理场多重信息的综合研究 ,可将东北东部地球物理及地质块体划分为A、B、C三类。它们在空间上有序的分布 ,特征上各自相异。揭示出所共处的区域岩石圈的大地构造环境演化历史的全过程。B类地块代表了太古宙陆块的形成 ;C类地块反映了古亚洲构造域复杂的造山过程 ;
Through the comprehensive study to the multiple information of the regional geologic physical field The geophysics and geological masses of eastern part of the Northeast can be divided into three classifications (A,B and C) In space,showing a regular distribution;in characteristics,showing various differences That revealed the whole evolutionary process of the geotectonic environment of the regional lithosphere The'B'mass indicated the forming of the Archeozoic landmass The'C'mass only indicated a complex orogenic process of the Paleo-Asiatictectonic domain The'A'mass revealed a post-Mesozoic dynamic process of the crust-mantle action-the decoupling process tectonism of the forming of basin-range structure,and the intense transformation of previous tectonism
出处
《吉林地质》
2002年第1期38-49,共12页
Jilin Geology
关键词
地球物理
地质块体
大地构造演化
中生代
壳幔作用
岩石圈
eastern part of Northeast
geophysics
geological mass
the evolution of the geotectology