n.各向異性(非均質(zhì)性)
The new method of structure geologic kinetics drawing is based on the positional anisotropism of the conductivity of ground geological products and water medium. 構(gòu)造地質(zhì)動(dòng)力制圖新方法的基礎(chǔ)是利用地表地質(zhì)生成物和水介質(zhì)導(dǎo)電性能的方位各向異性。
