摘要
为了使平衡剖面法具普遍性，在经典的几何平衡剖面法３原则基础上提出了物理平衡剖面法．该法的核心是岩层层面法线不变原则和变形匹配原则，兼顾了岩石变形的物理属性和几何属性．理论分析与实践结果表明，该法不仅可提高地质构造剖面的还原精度，而且可以简化地质分析，降低人为误差，提高自动化程度，更适合于大尺度、多期次构造变形剖面恢复．
The classical balanced cross section is essentially a method of geometry. To make it more available, we put forward the method of physical balanced cross sections on the basis of 3 rules of classical geometry balanced cross sections. Its kernel is the rule of the unchanged normal line of the layer surface and the deformation matching rule, with the consideration of all the physical and geometrical attributes. Theory analysis and practice reveal that it can not only enhance the recover accuracy of geological structures but also simplify geologic analysis, decrease manmade error, more automatic and more available for recovering large-scale, multi-times structure deformation.
出处
《地球科学（中国地质大学学报）》
EI
CAS
CSCD
北大核心
1998年第2期167-170,共4页
Earth Science-Journal of China University of Geosciences
基金
地质矿产部矿产资源定量预测及勘查评价开放研究实验室97项目
关键词
盆地模拟
物理平衡
剖面法
平衡剖面
地质构造
basin modeling, physical balanced cross section, balanced cross section, structure.
