摘要
中生代期间，中国东部的构造演变具有从西向东不断发展，从南向北不断扩展的特点。正是这种从南向北的构造演变与潮湿气侯带由南向北的不断迁移相结合，决定了中生代聚煤作用不断地从南向北迁移。
The characteristics of Mesozoic tectonic evolution in the eastern china is developing con-stantly from west to east and spreading consequently from south to nouth. It is because this tectonicevolution combingwith the wet climate zone migration from south to nouth that led to the Mesozoiccoal accumulation migration from south to nouth.
出处
《中国煤田地质》
1996年第2期5-8,19,共5页
Coal Geology of China
关键词
板块运动
构造演变
聚煤作用
中生代
煤矿床
Plate movement,tectonic evolution coal accumulation,Mesozoic age the eastern china
