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东准噶尔克拉麦里强应变构造带金的矿源层分维特征
引用本文:韩春明,陈川.东准噶尔克拉麦里强应变构造带金的矿源层分维特征[J].新疆地质,2000,18(2):177-180.
作者姓名:韩春明  陈川
作者单位:新疆工学院资源与环境工程系,新疆,乌鲁木齐,830008
摘    要:将分形几何学的原理和方法,应用于东准噶尔克拉麦里强应变构造带金的矿源层分维特征研究,发现在研究标度范围内金矿具有统计相似性,计算了研究区内金的矿源层的分维值,指出分维值与矿源层中的金品位呈正相关。

关 键 词:东准噶尔  矿源层  分维  金品位  强应变构造带
修稿时间:2000-01-28

FRACTAL DIMENSION CHARACTERISTICS OF THEGOLD IN THE OROGENIC BELT WITH STRONG STRAIN IN EAST JUNGGAR
HAN Chun-ming,CHEN Chuan.FRACTAL DIMENSION CHARACTERISTICS OF THEGOLD IN THE OROGENIC BELT WITH STRONG STRAIN IN EAST JUNGGAR[J].Xinjiang Geology,2000,18(2):177-180.
Authors:HAN Chun-ming  CHEN Chuan
Abstract:The principle and methods of fractal geometIy are applied to the study of fractal dimension of. the gold source bed in Kalamaili strong strained structure belt of east Junggar.We find that these gold souree beds possess statistical self-similar charateristics in the studied scale area,and the value of fractal di- mension of gold source bed are calculated. Moreover, we point out that the larger the values of gold source beds,the higher the Au grade.
Keywords:East Junggar  source bed fractal  dimension  Au  grade
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