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土壤地球化学测量在黄吉沟地区的找矿应用
引用本文:王玉,罗俊峰,谢刚. 土壤地球化学测量在黄吉沟地区的找矿应用[J]. 四川地质学报, 2014, 0(4): 628-631
作者姓名:王玉  罗俊峰  谢刚
作者单位:四川省地质矿产勘查开发局一〇九地质队,成都龙泉驿区610100
摘    要:通过对黄吉沟地区进行土壤地球化学测量,分别运用传统统计法和分形—求和法对Au、Cu、Bi、W的异常下限进行计算,并圈定了单元素异常图;确定了测区内的构造破碎带为Au、Cu有利富集区,而Bi、W与花岗岩密切相关。同时,在小范围尺度下,统计法在寻求主攻矿体时的作用明显,而分形法在矿体外围寻求找矿突破时实用性较强。

关 键 词:土壤地球化学测量  异常下限  找矿  黄吉沟

The Application of Pedogeochemical Survey to Prospecting in the Huangji Gully
WANG Yu,LUO Jun-feng,XIE Gang. The Application of Pedogeochemical Survey to Prospecting in the Huangji Gully[J]. Acta Geologica Sichuan, 2014, 0(4): 628-631
Authors:WANG Yu  LUO Jun-feng  XIE Gang
Affiliation:(No.109 Geological Team, BGEEMRSP, Chengdu 610100)
Abstract:The anomaly thresholds for Au, Cu, Bi, W elements are calculated by means of statistic method and fractal-summation method, and single element anomalies for Au, Cu, Bi, W are delineated on the basis of pedogeochemical survey data. The results indicate that enrichment in Au and Cu is related to fractured zone and Bi-W mineralization is related to granite rock mass.
Keywords:pedogeochemical survey  threshold  statistical method  fractal-summation method
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