刘普凯,卢飞,赵晓振.陕西凤县庞家河金矿床18号勘探线原生晕分带特征及深部预测[J].地质找矿论丛,2018,33(1):115-123
陕西凤县庞家河金矿床18号勘探线原生晕分带特征及深部预测
Primary halo zoning features along line 18 and deep ore prediction in Pangjiahe gold deposit, Fengxian county, Shanxi province
投稿时间:2016-10-14  
DOI:10.6053/j.issn.1001-1412.2018.01.015
中文关键词:  庞家河金矿  18号勘探线  地球化学特征  原生晕  深部预测  陕西
英文关键词:Pangjiahe Gold Deposit  exploration 18  geochemistry feature  primary halo  deepore prediction  Shanxi province
基金项目:陕西省地勘基金项目(编号:61201304171)资助。
作者单位
刘普凯 陕西省地质调查院, 西安 710065 
卢飞 中陕核工业集团211大队有限公司, 西安 710024
中国地质大学(武汉)资源学院, 武汉 430074 
赵晓振 中国地质大学(武汉)资源学院, 武汉 430074 
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中文摘要:
      庞家河金矿床地处秦岭造山带中西段的凤太多金属成矿带。矿区出露地层主要为泥盆系大草滩组,矿区构造类型多样,岩浆岩以花岗斑岩脉和辉绿岩脉为主。以原生叠加晕理论为指导,在矿区18号勘探线5个不同标高,采集了10种成矿元素的分析样品57件,通过对成矿元素统计学分析、原生晕轴向分带序列计算及各成矿元素异常分带特征研究,认为在庞家河矿区的18号勘探线深部矿体有较好的延伸。
英文摘要:
      Pangjiahe gold deposit is located at Fengtai polymetallic ore belt in the centralwest of Qinling orogenic belt. Devonian stratum, Dacaotan formation is mainly exposed in the mining area. The geological structure is complicated and magmatic rock is dominated by granite porphyry dykes and diabase dykes. This paper focuses on the 18th exploration line. Under guidance of the primary halo suoerimposition theory 57 samples are collected at the five different levels at 18th line to analyse the 10 different mineralization elements. We believe that ore body extents long to depth of 18th line through systamatic statistics analysis and the calculation of axial zoning sequence of primary halo.
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