中国东部中生代构造演变与聚煤作用的迁移  

MESOZOIC TECTONIC EVOLUTION AND COAL ACCUMULATION MIGRATION IN THE EASTERN CHINA

作　　者：陈传诗[1] 

机构地区：[1]焦作工学院

出　　处：《中国煤田地质》1996年第2期5-8,19,共5页Coal Geology of China

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.

关 键 词：板块运动 构造演变 聚煤作用 中生代 煤矿床 

分 类 号：P618.110.2[天文地球—矿床学]