论文部分内容阅读
以断裂构造地球化学为主,从常量元素-微量元素-稀土元素及其分异耗散顺序;矿物脉体-次生包裹体-同变形期流体及其微观动力学分析;压力强度-温热梯度-溶液浓度及其耦联相关体系;构造应力场-流变物理场-地球化学场及其参量数字模拟等4方面研究展望。上述4个方面既自成系统又相互关联,在时空演化上,可以结合地球动力学、构造年代学等统一解释。
Based on the tectono-geochemistry of faults, from the order of the major elements-trace elements-rare earth elements and their dissimilatory dissipative order; the mineral veins-secondary inclusions-the fluid during the same deformation period and its micro-dynamics analysis; the pressure intensity- Gradient - concentration of solution and its related systems; tectonic stress field - rheological physics - geochemical field and its digital simulation parameters 4 aspects of research prospects. The above four aspects are both self-contained and interrelated. In terms of temporal and spatial evolution, the above four aspects can be integrated with geodynamics and geochronology.