| 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 |
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| 引用本文： | 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. |
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| 作者姓名： | 刘普凯 卢飞 赵晓振 |
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| 作者单位： | 陕西省地质调查院;中陕核工业集团211大队有限公司;中国地质大学(武汉)资源学院; |
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| 基金项目： | 陕西省地勘基金项目（编号：61201304171）资助。 |
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| 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。
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| 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 |
| 收稿时间： | 2016/10/14 0:00:00 |
Primary halo zoning features along line 18 and deep ore prediction in Pangjiahe gold deposit, Fengxian county, Shanxi province |
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| LIU Pukai,LU Fei and ZHAO Xiaozhen.Primary halo zoning features along line 18 and deep ore prediction in Pangjiahe gold deposit, Fengxian county, Shanxi province[J].Contributions to Geology and Mineral Resources Research,2018,33(1):115-123. |
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| Authors: | LIU Pukai LU Fei and ZHAO Xiaozhen |
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| Institution: | Geological Survey of Shanxi Province, Xi''an, 710065,211 Geological Brigade of Sino Shanxi Nuclear Industry Group, Xi''an, 710024;China University of Geosciences(Wuhan), Wuhan, 430074 and China University of Geosciences(Wuhan), Wuhan, 430074 |
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| Abstract: | 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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| Keywords: | Pangjiahe Gold Deposit exploration 18 geochemistry feature primary halo deepore prediction Shanxi province |
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