现代地质
現代地質
현대지질
GEOSCIENCE-JOURNAL OF GRADUATE SCHOOL CHINA UNIVERSITY OF GEOSCIENCES
2014年
5期
942-952
,共11页
地球化学异常%传统统计学方法%85%累计频率%多重分形
地毬化學異常%傳統統計學方法%85%纍計頻率%多重分形
지구화학이상%전통통계학방법%85%루계빈솔%다중분형
geochemical anomaly%traditional statistical method%85% cumulative frequency method%multifractal
勘查地球化学的基础性问题是如何合理地提取地球化学异常下限,这是影响勘查地球化学在矿产勘查中效果的主要因素。利用 SPSS 软件,通过含量对数频率直方图,结合偏度、峰度检验法检验元素的含量分布型式,发现研究区的 Cu、Ag、Pb、Zn 元素不服从正态或对数正态分布,而呈现多峰态、高丛集的多重分形特征。采用传统的统计学方法、85%累计频率法、含量-总量多重分形法提取相关元素地球化学异常,并进行对比研究。研究结果表明,基于元素空间分布及含量分布规律的含量-总量多重分形方法,有效克服了传统方法的局限,比较客观地反映研究区的地球化学异常信息,是研究地球化学异常比较合理的方法。
勘查地毬化學的基礎性問題是如何閤理地提取地毬化學異常下限,這是影響勘查地毬化學在礦產勘查中效果的主要因素。利用 SPSS 軟件,通過含量對數頻率直方圖,結閤偏度、峰度檢驗法檢驗元素的含量分佈型式,髮現研究區的 Cu、Ag、Pb、Zn 元素不服從正態或對數正態分佈,而呈現多峰態、高叢集的多重分形特徵。採用傳統的統計學方法、85%纍計頻率法、含量-總量多重分形法提取相關元素地毬化學異常,併進行對比研究。研究結果錶明,基于元素空間分佈及含量分佈規律的含量-總量多重分形方法,有效剋服瞭傳統方法的跼限,比較客觀地反映研究區的地毬化學異常信息,是研究地毬化學異常比較閤理的方法。
감사지구화학적기출성문제시여하합리지제취지구화학이상하한,저시영향감사지구화학재광산감사중효과적주요인소。이용 SPSS 연건,통과함량대수빈솔직방도,결합편도、봉도검험법검험원소적함량분포형식,발현연구구적 Cu、Ag、Pb、Zn 원소불복종정태혹대수정태분포,이정현다봉태、고총집적다중분형특정。채용전통적통계학방법、85%루계빈솔법、함량-총량다중분형법제취상관원소지구화학이상,병진행대비연구。연구결과표명,기우원소공간분포급함량분포규률적함량-총량다중분형방법,유효극복료전통방법적국한,비교객관지반영연구구적지구화학이상신식,시연구지구화학이상비교합리적방법。
How to extract geochemistry anomalies reasonably is the fundamental question in the field of explora-tion geochemistry which is the key to the mineral exploration.In this study,we test the distribution characteris-tics of geochemical elements data by using the histogram of element contents and the testing method of skewness and kurtosis.The distribution characteristics of Cu,Ag,Pb and Zn did not follow the normal distribution and lognormal distribution,showing the characteristics of high cluster fractal distribution.This research compares the geochemical anomalies of related elements extracted by adopting traditional statistical method,the 85% cu-mulative frequency method and the content-gross multifractal method.The results show that the content-gross multifractal method based on the spatial distribution and content distribution of elements is relatively reasonable for studying geochemistry anomalies.This method overcomes the limitations of traditional methods effectively and reflects the information of geochemical anomalies objectively in the study area.