The early and middle Yanshanian tectonic movements permitted the fluvial, seasonal lake and intermittent lake facies to be developed.
受燕山早中期构造运动影响，河流相、时令湖相与间歇湖相发育。
2
The above shows that granulite facies metamorphism occurred in the crust of (increasing) thickness and caused by strong tectonic disturbance and regional high heat flow.
是麻粒岩相变质作用发生于地壳大幅度增厚的环境，强烈的构造变动和区域性高热流共同作用的结果。
3
Such a tectonic framework, in a great extent, controls the distribution of both the facies and thickness of coal-bearing sequences.