理想花岗岩显微图像中长石和石英的标度特性

Xu Deyi , Ke Xianzhong , Xie Shuyun , Cheng Qiuming
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引用次数: 0

摘要

本文利用在河北房山花岗岩体上采集的花岗岩样品的灰度显微图像,从分形的角度研究了长石和石英的性质。我们发现,长石和石英的灰度矩阵的特征值与其秩之间存在幂律关系。这里使用的分形模型是一个λ-R模型,类似于程秋明在2005年提出的N-λ模型。同时,我们发现在同一剖面上,长石的灰度基质的平均方差大于石英的灰度基质,这可能有助于长石和石英以及其他矿物的自动识别。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Scaling Properties of Feldspar and Quartz in Micro-images of Ideal Granites

The properties of feldspar and quartze are studied in this article from a fractal point of view using gray-scale micro-images of granite samples collected at the Fangshan granite body in Hebei Province, China, which can be regarded as an ideal granite in the sense of Vistelius. We found that there exist power-law relationships between the eigenvalues of the gray-scale matrices and their ranks for the feldspar and quartz. The fractal model used here is a λ-R model similar to the N-λ model proposed by Qiuming Cheng in 2005. Meanwhile, we found that average variances for the gray-scale matrices of feldspar are larger than those of quartz on the same sections, and this may be useful for auto-identification of feldspar and quartz as well as other minerals.

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