阿克陶县吐木艾尔克铅锌矿区元素回归分析

Regression Analysis of Elements in Tumuerke Lead-zinc Mining Area,Aketao County

吐木艾尔克铅锌矿位于新疆阿克陶县城东南约130 km处,距离英吉沙县城约100 km。它位于西昆仑地槽褶皱带的北缘,断裂破碎带控制着Pb、Zn、Fe、Cu等多金属矿带的分布。矿区位于铁克里克陆棚-断隆区石炭系卡拉巴西塔克组(C_(3)kl)。在前人基础地质研究的基础上,针对生产勘探中的部分基本分析样数据,本文应用多元线性回归方法,借助SPSS统计软件研究不同元素的品位关系,并建立线性回归方程,验证与解释吐木艾尔克铅锌矿硫化物矿床的成因与岩浆来源,这对应用数学地质方法有指引作用。

Tumuerke lead-zinc mine is located about 130 km southeast of Aketao County,Xinjiang,and about 100 km from Yingjisha County.It is located at the northern edge of the West Kunlun geotrough fold belt,and the fractured fracture zone controls the distribution of Pb,Zn,Fe,Cu and other polymetallic ore belts.The mining area is located in the Carboniferous Karabasitake Formation(C_(3)kl)in the Tieklik continental shelf-fault-uplift area.On the basis of previous basic geological research,aiming at some basic analysis sample data in production and exploration,this paper applies multiple linear regression method and uses SPSS statistical software to study the grade relationship of different elements,and establishes a linear regression equation to verify and explain the genesis and magma source of the sulfide deposit in the Tumuerke leadzinc deposit,which has a guiding role in the application of mathematical geological methods.