摘要
详细的构造－岩性填图研究表明，恒山变质岩区存在五台群的基底杂岩，该区晚太古代一早元古宙经历了表壳岩形成－深成岩体侵位事件，并且涉及多期构造变形（褶皱、剪切作用）与变质。其中，大规模近水平剪切变形造成基底杂岩的不同单位构造叠置和重熔。地质事件序列记录了恒山地区早前寒武纪陆壳生长、分异的克拉通化过程及大陆裂谷作用。
Detailed structural-lithologic mapping in typical sectors of the Hengshan metamorphicterrain indicates that there exist basement compleses of the Archean Wutai Group in the ter-rain. During the Late Archean to Early Proterozoic the terrain undrwent the event of formationof supracrustal sequences and emplacement of plutons and polyphase structural deformauon(folding and shearing) and metamorphism. Among other things, large- scale subhorizontalshearing resulted in superimposition of different structural units and anatexis of basement com-plexes. Geological events series recorded accretion, differentiation and finally cratonization ofthe continental crust and subsequent continental rifiting in the Early Precambrian in the Heng-shan area.
出处
《中国区域地质》
CSCD
1995年第1期36-43,共8页
Regional Geology of China
基金
国家自然科学基金资助项目
