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现代地质 ›› 2016, Vol. 30 ›› Issue (4): 811-817.

• 地球化学 • 上一篇    下一篇

基于MAPGIS的含量-面积分形法确定元素异常下限及圈定异常区:以湖南阳明山地区为例

崔玉良1,2,王根厚2,郎欣欣3,曾志方4   

  1. 1北京探矿工程研究所,北京100083;2中国地质大学(北京)地球科学与资源学院,北京100083 3内蒙古自治区第十地质矿产勘查开发院,内蒙古 赤峰024005;4湖南省地质矿产勘查开发局四○九队,湖南 永州425000;
  • 出版日期:2016-08-31 发布日期:2016-09-08
  • 通讯作者: 王根厚,男,教授,博士生导师,1963年出生,构造地质学专业,长期从事构造地质学的教学与科研工作
  • 作者简介:崔玉良,男,硕士研究生,1989年出生,构造地质学专业,主要从事构造地质学研究。
  • 基金资助:
    中国地质调查局项目(1212011220522)

Determination of the Element Anomaly Threshold and the Enclosed Abnormal Area by Using ContentArea Fractal Method Based on MAPGIS:Exampled by Yangmingshan Area of Hunan Province

CUI Yuliang1,2, WANG Genhou2, LANG Xinxin3, ZENG Zhifang4   

  1. 1Beijing Institute of Exploration Engineering,Beijing100083, China;2School of Earth Sciences and Resources, China University of Geosciences, Beijing100083, China;3Inner Mongolia Tenth Geological Mineral Exploration Institute, Chifeng, Inner Mongolia024005,China; 4409 Team, Bureau of Geology and Mineral Exploration and Development of Hunan, Yongzhou, Hunan425000, China
  • Online:2016-08-31 Published:2016-09-08

摘要: 地球化学元素的异常下限值确定是地球化学中重要的问题之一,目前还没有一个完善的具有科学依据的计算方法。传统的化探异常下限值计算是以元素含量或元素含量的对数值呈正态分布这一假设为基础的,而事实上地球化学元素含量的空间分布是极其复杂的。研究表明,地球化学景观可能是一个具有低维吸引子的混沌系统,元素的地球化学背景值和异常具有各自独立的幂指数关系,由此导致了一种多重分形分布,可以利用元素的分形分布求出其异常下限。对湖南省阳明山地区的化探水系采样分析数据采用分区的处理方法,根据每个区内数据的分布特征采用分形和传统方法混合应用来确定异常下限,勾绘出Sn元素异常图,与单独采用传统方法相对比收到了良好的异常圈定效果。根据新方法确定的元素异常下限所圈定的异常区与已知矿点高度拟合。

关键词: 元素异常下限, 含量-面积, MAPGIS, 湖南省阳明山

Abstract: The determination of thresholds of chemical elements is one of the important problems in geochemical exploration. At present, there is not a scientific way to confirm the thresholds.The traditional way to determine the thresholds of chemical elements is based on the assumption of normal distribution of the element contents or their logarithms. In fact,the space distribution of geochemical element content is extremely complex; and the studies showed that the geochemical landscape may be a lowdimensional chaotic attractor system. The background values and anomalies of the elements have their own exponential relationship, which lead to a multifractal distribution, thus obtaining the anomaly threshold of element through the distribution of fractal elements. In this paper, the method of dividing area of geochemical exploration sample analysis data in Yangmingshan in Hunan is adopted. The threshold is determined through mixed application of fractal and traditional methods according to the distribution of data,drawing out the Sn anomaly map. It obtained better performance than by using the traditional method only, and the abnormal area enclosed by the element anomaly thresholds which is determined by the new method highly conformed to the known ore spots.

Key words: element anomaly threshold, contentarea, MAPGIS, Yanmingshan area of Hunan Province

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