陕西金龙山金矿古楼山矿段元素地球化学特征

J4 ›› 2011, Vol. 19 ›› Issue (1): 28-33.

陕西金龙山金矿古楼山矿段元素地球化学特征

陈力子，曹东宏，杨登美

武警黄金第五支队

出版日期:2011-02-28 发布日期:2012-03-16
通讯作者: 陈力子（1973-），男，山东成武人，工程师，从事地球化学找矿工作.chleezi@yahoo.com.cn

Element Geochemical Characteristics of Guloushan Ore Section in Jinlongshan Gold Mine,Shaanxi Province

Online:2011-02-28 Published:2012-03-16

摘要/Abstract

摘要：

古楼山矿段位于金龙山金矿田的西北部，与丘岭矿段处于同一地球化学异常中，是另一异常浓集中心，目前在丘岭矿段已探明储量超过50 t，古楼山矿段由于工作程度较低，未取得大的突破。通过对古楼山矿段原生晕的分析，发现原生晕中As、Sb、Au元素相关性高且呈正相关关系，表明As、Sb、Au为该区金矿预测的主要元素组合，建立了地球化学原生晕理想模式，元素组合特征表明在该矿段的下部还有较大的找矿空间。

关键词: 古楼山矿段, 地球化学特征, 找矿意义, 金龙山金矿田

Abstract:

Guloushan ore section is located in the northwest of Jinlongshan gold deposit,at present the reserves of Qiuling ore section has been beyond 50 t.Since research degree is lower,there is not got big breakthrough in Guloushan ore section.Through analysis of the Guloushan ore section primary halo,As,Sb and Au elements association has higher correlation and the correlational dependence,it indicate the main elements association of the gold deposit principal in this place are As,Sb and Au element,and we establish a geochemical primary halo ideal model,the characteristics of elemental association indicate that there are quite exploration space in the lower part of the ore section.

Key words: Guloushan ore section, Geochemistry characteristic, Prospecting significance, Jinlongshan gold field

陈力子, 曹东宏, 杨登美. 陕西金龙山金矿古楼山矿段元素地球化学特征[J]. J4, 2011, 19(1): 28-33.

CHEN Li-Zi, CAO Dong-Hong, YANG De-Mei. Element Geochemical Characteristics of Guloushan Ore Section in Jinlongshan Gold Mine,Shaanxi Province[J]. J4, 2011, 19(1): 28-33.

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