摘要
本文在九瑞矿集区区域瑞昌旋卷构造、矿田控矿构造型式及地球化学形迹分析的基础上,以流体运动学理论、涡旋场强间的几何相容关系和三维流动涡旋场的非线性耦合原理为依据,研究分析了块状硫化物型矿体涡旋成矿作用控制机理,较圆满解释了围绕城门山、武山主成矿岩体东、西两端的块状硫化物型矿体在在的空间分布、成矿元素组合的不对称差异,表明其是受控于涡旋成矿作用的结果。
In this thesis, on the basic of analysis of Jiujiang - Ruichang metallogenic district Rulichang vortex structure, ore - controlling structure and geochemistry features, according to the theory of fluid kinematics, geometric compatibility be- tween the vortex fields strength and three - dimensional flow of the vortex field nonlinear coupling principle, we have studied the mineralization of massive sulfide orebody vortex control mechanism and got a satisfactory explanation of why the massive sulfide ore body has asymmetry differences in spatial distribution and ore -forming elements,that distribute on both ends of east and west in main metallogenie ore body around Chengmenshan and Wushan ore fields. All of these indicated it is con- trolled by the vortex mineralization result.
出处
《江西化工》
2016年第1期80-84,共5页
Jiangxi Chemical Industry
关键词
矿集区
块状硫化物
成矿流体
涡旋
成矿作用
Metallogenic Distrlct
massive sulfide
ore - forming fluid
vortex
mineralization
