Primary Halo Characteristics of the Orebody in Dahu Gold Deposit，Xiaoqinling Area

SUN Baohua; NIU Shuyin; WANG Xingcun; SUN Aiqun; DING Peichao; LI Qiangfeng; HOU Jianglong

doi:10.11872/j.issn.1005-2518.2014.04.055

Gold Science and Technology >

2014 , Vol. 22 >Issue 4: 55 - 60

DOI: https://doi.org/10.11872/j.issn.1005-2518.2014.04.055

Primary Halo Characteristics of the Orebody in Dahu Gold Deposit，Xiaoqinling Area

SUN Baohua ,
NIU Shuyin ,
WANG Xingcun ,
SUN Aiqun ,
DING Peichao ,
LI Qiangfeng ,
HOU Jianglong

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1.Shijiazhuang University of Economics，Shijiazhuang 050031，Hebei，China；
2.The First Geological Survey Institute of Henan Geological Exploration and Exploitation Bureau，Luoyang 471023，Henan，China

Received date: 2014-05-30

Revised date: 2014-07-01

Online published: 2014-12-24

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Abstract

The deposit geochemical primary halo axial zonation is an important basis to predict of deep ore body.Gold mineralization is superimposed with characteristics of multi-phase and multi-stage in Dahu gold deposit.Anomalies combination of geochemical elements in different elevation is different of location of orebody.This paper focuses on content of Au，Ag，Co，Cu，Mn，Mo，Ni，Pb and other 18 kinds of elements in No.17，19 and 22 orebody in the F5 structural zone in Dahu gold mine and altered rocks，we do the correlation analysis and poly class analysis，and focuses on the characteristics of their primary halo.We takes the Xiaoqinling gold field structural superimposed halo ideal model as a reference to explain the characteristics of the orebody primary halos，it is believed that the elongation of No.19 orebody is not very long.To write this paper，we except to provide a reference for deep gold mine prospecting and exploration of other fields in Xiaoqinling.

Key words： correlation analysis; cluster analysis; structural superimpose halo; geochemistry; Xiaoqinling gold field

Cite this article

SUN Baohua , NIU Shuyin , WANG Xingcun , SUN Aiqun , DING Peichao , LI Qiangfeng , HOU Jianglong . Primary Halo Characteristics of the Orebody in Dahu Gold Deposit，Xiaoqinling Area[J]. Gold Science and Technology, 2014 , 22(4) : 55 -60 . DOI: 10.11872/j.issn.1005-2518.2014.04.055

References

［1］戚开静.小秦岭金矿田成矿规律与成矿预测［D］.北京：中国地质大学（北京），2010.
［2］王杏村，牛树银，燕建设，等.小秦玲中矿带金矿田成矿构造分布［J］.黄金科学技术，2012，20（4）：96-103.
［3］卿敏，刘连登.小秦岭不同性质剪切带与金矿的时空关系及其找矿意义［J］.黄金科学技术，1995，3（2）：17-20.
［4］谭满堂.小秦岭地区金矿构造控矿规律［D］.武汉：中国地质大学（武汉），2013.
［5］冯建之.河南小秦岭金矿构造控矿规律及控矿模式［J］.矿产与地质， 2009，23（4）：302-307.
［6］何春芬.小秦岭金矿田北矿带F5断裂控矿作用［J］.黄金，2003，24（9）：3-7.
［7］杨继红，张进春，苗翠梅.小秦岭大湖金矿区F5控矿规律及其应用研究［J］.河南理工大学学报（自然科学版），2007，26（6）：659-663.
［8］李晓波，刘继顺.小秦岭大湖金矿床的矿化分带规律及其指示意义［J］.地质找矿论丛， 2003， 18（4）：243-248.
［9］孙卫志，王振强.小秦岭大湖矿区钼、金矿体地质、地球化学特征与差异性分析［J］.地质论评，2012，58（4）：671-680 .
［10］李惠，李德亮，禹斌，等.构造叠加晕新方法在小秦岭金矿带深部盲矿预测的应用［J］.黄金科学技术，2010，18（5）：1-6.

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