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不同地质空间有其自身的发展过程和沉积间断史.在编制辽宁省大地构造图的过程中,我们根据相邻地质空间地质发展过程的同异,划分了Ⅰ～V级构造单元. 全省共划分出Ⅰ级构造单元2个,Ⅱ级4个,Ⅲ级11个,Ⅳ级24个,V级31个.本次矢量分析只做到Ⅲ级构造单元.Ⅰ、Ⅱ、Ⅲ级构造单元的名称见图. 既然不同地质空间即不同构造单元沉积间断存在着差异,或者上升遭到剥蚀,或者下降接受沉积,这种升降对矿产形成后的影响,就是区域找矿工作中不可忽视的一个问
Different geological space has its own development process and discontinuous sedimentary history.In the process of compiling the tectonic map of Liaoning Province, we classify the Ⅰ ~ V tectonic units according to the similarities and differences of the geological development process of the adjacent geological space. Divided into I-level structural units 2, Ⅱ 4, Ⅲ 11, Ⅳ 24, V 31. This vector analysis only to the third-level structural units.Ⅰ, Ⅱ, Ⅲ-level structural units The name see Figure Since the different geological space that is different between the structural units of sedimentary differences exist, or rose to be denuded or declined to accept deposition, the rise and fall of mineral formation after the impact of the regional prospecting work can not be ignored