摘要
燕山运动在浙江及华南各省普遍存在，对其阶段（期）的划分尚有一些分歧。近年对浙江省岩石地层单位及构造运动不整合面进行了清理，将中生代构造运动划分为５个阶段。建议把印支运动之后至白垩纪末期的地壳运动称为广义的燕山期，而把狭义的燕山运动置于白垩纪末期。
The Yanshan movement was prevalent in Zhejiang and various provinces of South China, but there are still some divergent views about its stages. Through purification of the lithostratigraphic units and unconformities of tectonic movements, the Mesozoic tectonic movements are divided into five stages. The authors suggest that the crustal movement after the Indosinian movement till the terminal Cretaceous is called the Yanshanian tectonic stage sensus lato, while the Yanshanian movement sensus stricto is assigned to the terminal Cretaceous. The Fujian-Zhejiang movement will continue to be used.
出处
《中国区域地质》
CSCD
1999年第2期201-204,共4页
Regional Geology of China
