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    云南北衙铁金矿区小波多尺度分析综合解释方法应用效果

    曾琴琴, 王永华, 杨剑

    曾琴琴, 王永华, 杨剑. 云南北衙铁金矿区小波多尺度分析综合解释方法应用效果[J]. 沉积与特提斯地质, 2012, 32(4): 100-105.
    引用本文: 曾琴琴, 王永华, 杨剑. 云南北衙铁金矿区小波多尺度分析综合解释方法应用效果[J]. 沉积与特提斯地质, 2012, 32(4): 100-105.
    ZENG Qin-qin, WANG Yong-hua, YANG Jian. Application of the multi-scale wavelet analytical method: A case study of the Beiya iron-gold mining district in Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(4): 100-105.
    Citation: ZENG Qin-qin, WANG Yong-hua, YANG Jian. Application of the multi-scale wavelet analytical method: A case study of the Beiya iron-gold mining district in Yunnan[J]. Sedimentary Geology and Tethyan Geology, 2012, 32(4): 100-105.

    云南北衙铁金矿区小波多尺度分析综合解释方法应用效果

    基金项目: 

    北衙金矿远景区深部调查评价(项目编号:1212011220249)

    详细信息
      作者简介:

      曾琴琴(1982-),女,博士,主要从事地球物理数据处理及方法技术研究。E-mail:162039179@qq.com

    • 中图分类号: P631.1

    Application of the multi-scale wavelet analytical method: A case study of the Beiya iron-gold mining district in Yunnan

    • 摘要: 通过模型磁异常分解,结合功率谱分析及异常振幅计算场源深度并判断场源分布平面位置,表明小波多尺度分析在位场分离中的有效性。将该方法应用于北衙铁金矿区磁异常分析解释,通过功率谱分析估算了各阶细节及四阶逼近的场源深度,结合不同深度异常振幅推断了磁源空间展布关系特征。分析表明,区内北部和西部强磁异常主要由矿体引起,且矿体在中深部产状发生改变;而东部大范围磁异常区主要为二叠系玄武岩所致。
      Abstract: The calculation of the depths of field sources and the determination of the planar distribution of field sources based on the model for the decomposition of magnetic anomalies, power spectrum analysis and abnormal amplitudes indicate the effectiveness of multi-scale wavelet analytical method on potential field separation. In this paper, the method is applied to analyze and interpret the magnetic anomalies in the Beiya iron-gold mining district, Heqing, Yunnan. The emphasis is placed on the calculation of the depths of field sources of each order details and 4th-order approximation on the basis of power spectrum analysis, and the determination of spatial distribution of magnetic sources inferred from the abnormal amplitudes at varying depths. The results in this study show that the orebodies are responsible for highly magnetic anomalies in the northern and western parts of the Beiya iron-gold mining district, and display the modification in occurrence at the medium-deep parts of it. The wide ranges of magnetic anomalies in the eastern part of it are caused by the Permian basalts. The results outlined above may inspire some new approaches to the further deep-seated exploration and development in the study area.
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    出版历程
    • 收稿日期:  2012-07-24
    • 修回日期:  2012-09-29
    • 发布日期:  2012-12-29

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