金属矿山
金屬礦山
금속광산
METAL MINE
2015年
2期
98-102
,共5页
李静静%阳正熙%李文娟%陈飞%班建永%刘磊
李靜靜%暘正熙%李文娟%陳飛%班建永%劉磊
리정정%양정희%리문연%진비%반건영%류뢰
金多金属矿床%土壤地球化学特征%元素异常组合%异常下限%找矿预测
金多金屬礦床%土壤地毬化學特徵%元素異常組閤%異常下限%找礦預測
금다금속광상%토양지구화학특정%원소이상조합%이상하한%조광예측
Gold-polymetallic deposit%Soil geochemical characteristics%Element anomaly combination%Anomaly thresh-old%Ore-prospecting
通过在山西洞沟多金属矿区开展1∶10000土壤地球化学测量工作,首先对测量数据的统计特征进行分析;然后利用Spss软件对其进行相关分析、聚类分析和因子分析,在此基础上确定出工作区内的元素异常组合;最后利用Spss软件作出各元素的盒须图,求出其第1个四分位数和第3个四分位数,从而确定出各元素的异常下限。结果表明:①Au、Ag、Hg、As、Sb、Bi、Ba、Pb、Zn、W等元素含量较高,变异系数较大,具有一定的次生富集倾向;②Ag、Pb、Zn、Mo、Au、Hg、Ba、W等元素代表主要成矿元素的次生富集组合;③通过确定异常下限及圈定各元素异常可知,异常较高的元素均分布在矿区的中部或东部且在构造破碎带内。上述研究结果对于区内进一步开展找矿工作具有一定的指导作用。
通過在山西洞溝多金屬礦區開展1∶10000土壤地毬化學測量工作,首先對測量數據的統計特徵進行分析;然後利用Spss軟件對其進行相關分析、聚類分析和因子分析,在此基礎上確定齣工作區內的元素異常組閤;最後利用Spss軟件作齣各元素的盒鬚圖,求齣其第1箇四分位數和第3箇四分位數,從而確定齣各元素的異常下限。結果錶明:①Au、Ag、Hg、As、Sb、Bi、Ba、Pb、Zn、W等元素含量較高,變異繫數較大,具有一定的次生富集傾嚮;②Ag、Pb、Zn、Mo、Au、Hg、Ba、W等元素代錶主要成礦元素的次生富集組閤;③通過確定異常下限及圈定各元素異常可知,異常較高的元素均分佈在礦區的中部或東部且在構造破碎帶內。上述研究結果對于區內進一步開展找礦工作具有一定的指導作用。
통과재산서동구다금속광구개전1∶10000토양지구화학측량공작,수선대측량수거적통계특정진행분석;연후이용Spss연건대기진행상관분석、취류분석화인자분석,재차기출상학정출공작구내적원소이상조합;최후이용Spss연건작출각원소적합수도,구출기제1개사분위수화제3개사분위수,종이학정출각원소적이상하한。결과표명:①Au、Ag、Hg、As、Sb、Bi、Ba、Pb、Zn、W등원소함량교고,변이계수교대,구유일정적차생부집경향;②Ag、Pb、Zn、Mo、Au、Hg、Ba、W등원소대표주요성광원소적차생부집조합;③통과학정이상하한급권정각원소이상가지,이상교고적원소균분포재광구적중부혹동부차재구조파쇄대내。상술연구결과대우구내진일보개전조광공작구유일정적지도작용。
Through conducting the soil geochemical survey work in a scale of 1 ∶ 10 000 in Donggou gold-polymetallic deposit area,the statistical characteristics of the survey data is firstly analyzed,and then,the survey data is conducted on corre-lation analysis,cluster analysis and factor analysis based on Spass software so as to obtain the element anomaly combination in the mining area;Finally,the Spass software is adopted to make the box plot of each element so as to determine the anomaly thresholds of each element by obtaining the first quartile and third quartile. The research results show that:①the elements such as Au,Ag,Hg,As,Sb,Bi,Ba,Pb,Zn and W have a certain tendency of secondary enrichment because its contents are higher than other elements relatively,and its coefficients of variation are larger than that of other elements;②the elements such as Ag,Pb,Zn,Mo,Au,Hg,Ba and W elements represent the secondary enrichment combination of the main ore-forming elements;③it is obvious that the high abnormal elements distribute in the central or the eastern part of the mining area and within the tectonic fracture zone by determining the abnormal threshold and selecting the elements′anomalies. The above results can pro-vide some reference for the ore-prospecting work in the mining area.