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.
發文機構:SchoolofArchitecture GuangzhouInstituteofGeochemistry
關鍵詞:巖石斷層動力學分析反作用-力傳遞-機械力關聯非線形關聯動力模型非規則發展斷層特性reaction-transport-mechanical couplingcomplexitychaotic evolutionrock faulting
分類號: P541[天文地球—構造地質學][天文地球—地質學]P584[天文地球—巖石學][天文地球—地質學]