摘要
本文首次把分形分维技术应用到岩矿石激发极化时间谱资料的处理中，并建立了相应的分形分维弛豫模型．通过大量和系统的理论与实验研究，得出了一些有意义的结论和认识．
おor the first time,we applied fractal dimension technique to the field of time-domain IP decay of mineralized rock,and also set up relevant fractal dimension relaxation model. Through a large number and systematic experimental、theoretical study,we obtaied some significant conclusions and understandings.
出处
《地球物理学进展》
CSCD
1998年第1期79-83,共5页
Progress in Geophysics
关键词
分形
激电时间谱
激发极化法
分形几何
岩矿石
fractal dimension,Self-similary,Time-domain IP,Fractal relaxation model
