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Multifractal Analysis of Element Distribution in Skarn-type Deposits in the Shizishan Orefield, Tongling Area, Anhui Province, China

WANG Qingfei DENG Jun WAN Li ZHAO Jie GONG Qingjie YANG Liqiang ZHOU Lei ZHANG Zhijun

地质学报(英文版)2008,Vol.82Issue(4):896-905,10.
地质学报(英文版)2008,Vol.82Issue(4):896-905,10.

Multifractal Analysis of Element Distribution in Skarn-type Deposits in the Shizishan Orefield, Tongling Area, Anhui Province, China

Multifractal Analysis of Element Distribution in Skarn-type Deposits in the Shizishan Orefield, Tongling Area, Anhui Province, China

WANG Qingfei 1DENG Jun 2WAN Li 1ZHAO Jie 2GONG Qingjie 1YANG Liqiang 3ZHOU Lei 1ZHANG Zhijun2

作者信息

  • 1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences,Beijing 100083, China
  • 2. Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education, China University of Geosciences, Beijin
  • 3. School of Mathematics and Information Science, Guangzhou University, Guangzhou, Guangdong 510405, China
  • 折叠

摘要

Abstract

A series of element concentrations sampled from four drill cores with a length about 1000 minto different skarn.type deposits were selected from the Shizishan orefield, central Tongling,southeastern part of Anhui Province. Using the multifractal method, the distribution and migrationcharacteristics of the major and trace elements are analyzed. The multifractai spectrum of the majorelements is left-skewed, whereas the spectrum of the trace elements is right-skewed, which shows thatin the process of skaru formation, the trace elements were enriched only locally, and major elementstransported within a much larger range. The correlation coefficients of the multifractai parametersAa (width of the multifractal spectrum) of the four drill cores are relatively low, but the correlationcoefficients of the multifractal parameters R (spectrum symmetry parameter) and Af are relativelyhigher, indicating that although the non-homogeneous intensity of the distribution of elements isinconsistent, their spatial accumulation patterns are almost the same during the ore-forming process.The statistics of the multifractal parameters of various elements in the different locations show thatthe ore-forming processes and element migration pattern in the Shizishan orefield are consistent, andthat the migrations of trace elements and major elements exhibit some differences.

关键词

metallogenie elements, skarn, mnltifractal spectrum, Tongling, Anhui, China

Key words

metallogenie elements, skarn, mnltifractal spectrum, Tongling, Anhui, China

分类

天文与地球科学

引用本文复制引用

WANG Qingfei,DENG Jun,WAN Li,ZHAO Jie,GONG Qingjie,YANG Liqiang,ZHOU Lei,ZHANG Zhijun..Multifractal Analysis of Element Distribution in Skarn-type Deposits in the Shizishan Orefield, Tongling Area, Anhui Province, China[J].地质学报(英文版),2008,82(4):896-905,10.

基金项目

This research was supported by the Special Plans of Science and Technology of the Land Resources Department (No.20010103):the Trans-century Training Program Foundation of the Ministry of Education (No.20010103)

and the 111 Project (No.B07011). (No.B07011)

地质学报(英文版)

OACSCD

1000-9515

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