CNN Modeling for the Periodic Banding Texture of Sphalerite
Under the hypothesis that the crystallization process for forming sphalerite banding textures occurs in the plane perpendicular to the axis of calcium carbonate crystal in a hexagon area and the reaction-diffusion process is from outside of the system area inward, a CNN model is built to simulate the periodic banding textures of sphalerite based on the dynamic model suggested by Sergei Katsev and Ivan LHeureux in 2001. The simulated results meet with some observations quite well, which implies that our hypothesis is reasonable and the CNN model can be used to interpret the mechanism for the forming of various textures of sphalerite.
Deyi Xu Qiuming Cheng Zhijing Wang
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Department of Earth and Space Science and Engineering, York University, M3J 1P3, Toronto, Canada
国际会议
The 12th Conference of the International Association for Mathematical Geology(第12届国际数学地质大会)
北京
英文
224-226
2007-08-26（万方平台首次上网日期，不代表论文的发表时间）