作者:TANKaixuan,XIEYanshi,CHENGuanghao,HUANGXiaonai
摘要:Fault is a complex dynamic system controlled by the coupling of rock texture, reaction, fluid flow,stress, and rock deformation mechanism. A coupled reaction-transport- mechanical dynamic model for fault system is established and described in this paper. An example is presented for the Shuikoushan deposit, Hunan. The results of dynamic simulation indicate that the evolution and magnitude of fracture permeability of different rocks are different, and that faulting can enhance the spatial heterogeneity of rock permeability and facilitate fluid flow and mineralization in local fault zone. The pressure for a fault usually shows a variation mode of aperiodic oscillation with time, which reflects the chaotic behavior of the evolution of a fault.
发文机构:SchoolofArchitecture GuangzhouInstituteofGeochemistry
关键词:岩石断层动力学分析反作用-力传递-机械力关联非线形关联动力模型非规则发展断层特性reaction-transport-mechanical couplingcomplexitychaotic evolutionrock faulting
分类号: P541[天文地球—构造地质学][天文地球—地质学]P584[天文地球—岩石学][天文地球—地质学]