构造-流体耦合有限元模拟:以石英脉型钨矿为例
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摘要
热液矿床成矿作用动力学过程涉及多时空高度耦合的物理和化学过程。数值模拟是研究这一复杂动力学过程的重要而有效的工具之一,也可在找矿预测等方面发挥重要作用。以南岭地区石英脉钨矿床为例,利用计算机求解控制构造-流体的物理和化学方程,定量揭示成矿热液聚焦流动与"五层楼"成矿的对应关系,正演高压成矿流体致使围岩发生水力破裂及其成矿效应。模拟结果与石英脉型钨矿床的构造地球化学特征相符。
The dynamic process of hydrothermal ore-forming involves highly coupled physical and chemical processes at different spatial and temporal scales. Numerical simulation is one of important and effective tools to decipher these complex processes and aids in prospecting. The vein-type tungsten deposits in the Nanling Range are taken examples to show how to solve the physical and chemical equations controlling the coupled structure-fluids using numerical simulation,decipher the relationships between fluid focusing and the tungsten mineralization in the five-floor vertically morphological zonation quantitatively,and reproduce the influences of hydraulic fracturing driven by high-pressure fluids on wolframite precipitation. The numerical results are consistent with the geochemical characteristics constrained by previous studies.
The dynamic process of hydrothermal ore-forming involves highly coupled physical and chemical processes at different spatial and temporal scales. Numerical simulation is one of important and effective tools to decipher these complex processes and aids in prospecting. The vein-type tungsten deposits in the Nanling Range are taken examples to show how to solve the physical and chemical equations controlling the coupled structure-fluids using numerical simulation,decipher the relationships between fluid focusing and the tungsten mineralization in the five-floor vertically morphological zonation quantitatively,and reproduce the influences of hydraulic fracturing driven by high-pressure fluids on wolframite precipitation. The numerical results are consistent with the geochemical characteristics constrained by previous studies.
引文
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[7]王偲瑞,杨立强,孔鹏飞.焦家断裂渗透性结构与金矿床群聚机理:构造应力转移模拟[J].岩石学报,2016,32(8):2494-2508.WANG Sirui,YANG Liqiang,KONG Pengfei.Permeability structure and gold deposits cluster mechanism along the Jiaojia fault,China:Structure stress transfer modeling[J].Acta Petrologica Sinica,2016,32(8):2494-2508.(in Chinese with English abstract)
[8]刘亮明,周瑞超,赵崇斌.构造应力环境对浅成岩体成矿系统的制约:从安庆月山岩体冷却过程动力学计算模拟结果分析[J].岩石学报,2010,26(9):2869-2878.LIU Liangming,ZHOU Ruichao,ZHAO Chongbin.Constraints of tectonic stress regime on mineralization system related to the hypabyssal intrusion:Implication from the computational modeling experiments on the geodynamics during cooling process of the Yuenshan intrusion in Anqing district,China[J].Acta Petrologica Sinica,2010,26(9):2869-2878.(in Chinese with English abstract)
[9]LI X H,YUAN F,ZHANG M M,et al.3D computational simulation-based mineral prospectivity modeling for exploration for concealed Fe-Cu skarn-type mineralization within the Yueshan orefield,Anqing district,Anhui Province,China[J].Ore Geology Reviews,2019,105:1-17.
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[12]LIU X C,MA Y,XING H L,et al.Chemical responses to hydraulic fracturing and wolframite precipitation in the veintype tungsten deposits of southern China[J].Ore Geology Reviews,2018,102:44-58.
[13]LIU X C,XING H L,ZHANG D H.The mechanisms and time scale of alteration halos in vein-type tungsten deposits in southern China[J].Ore Geology Reviews,2017,89:1019-1029.
[14]XING Huilin.Finite element modelling of biogas process from coal[J].Chinese Journal of Computational Mechanics,2016,33(4):637-642.
[15]古菊云.华南钨矿脉的形态分类[C]//余鸿彰.钨矿地质讨论会论文集.北京:地质出版社,1984:35-45.GU Jiyun.Morphological zonation of tungsten deposits in South China[C]//YU Hongzhang.Proceedings of Symposium on Tungsten Geology.Beijing:Geological Publishing House,1984:35-45.(in Chinese)
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