王仔章,刘铭.综合地球物理勘探在夏日哈木矿区的应用研究[J].地质找矿论丛,2022,37(1):103-110
综合地球物理勘探在夏日哈木矿区的应用研究
Application research on integrated geophysical exploration in Xiarihamu mining area
投稿时间:2021-02-25  
DOI:10.6053/j.issn.1001-1412.2022.01.014
中文关键词:  地球物理勘探  铜镍矿床  夏日哈木矿区  青海省
英文关键词:geophysical exploration  Cu-Ni deposit  Xiarihamu mining area  Qinghai province
基金项目:青海省地矿局项目(编号:2014-56)资助。
作者单位
王仔章 河南中核五院研究设计有限公司, 郑州 450052 
刘铭 山东省鲁南地质工程勘察院, 山东 济宁 272008
山东省地勘局第二地质大队, 山东 济宁 272008 
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中文摘要:
      文章通过选用高精度磁测剖面测量、激电中梯剖面测量、高精度重力剖面测量、可控源音频大地电磁测深等方法对青海省夏日哈木铜镍矿床开展地球物理方面的研究,探讨各种物探手段对该区矿床勘查的有效性及适用性,丰富区内物探资料,为区内同类型矿床勘查提供借鉴。研究表明,高精度磁测剖面测量在大范围寻找矿体较为有效,但难以表达矿体的形态特征;激电中梯剖面测量中极化率曲线能准确定位矿体的位置、显示矿体的规模,在一定程度上反映矿体的展布特征;高精度重力剖面测量中布格重力曲线与剩余异常曲线均能表现相对高异常,异常曲线在一定程度上反映矿体的位置及大致规模;可控源音频大地电磁测深方法对铜镍矿床进行勘查时,能较为准确地反映矿体的深部特征,尤其是反射系数图,能准确对深部盲矿体进行表达。
英文摘要:
      High precision magnetic survey profile measurement,IP intermediate gradient profile measurement,high precision gravity profile measurement and controllable source audio magneto telluric sounding survey are integratedly operated in Xiharihamu Cu-Ni deposit in Qinghai province to research on effectiveness and applicability of the above each geophysical techniques and provide data and references for prospecting similar ore deposits in the area.The results show that the high precision magnetic survey profile measurement is relatively effective for prospecting ore bodies in large area but can not display morphological feature of ore bodies.The Polarisability curve of IP intermediate profile measurement can be prepared to locate position of ore body and display it's size and the distribution feature to a certain extent.Both Bouguer gravity curve and residual anomaly curve of high precision gravity profile measurement show relatively high anomaly and the anomaly curve shows ore body position and it's size to a certain degree.For prospecting Cu-Ni deposit the controllable source audio magnetotelluric sounding technique can be prepared to reflect characteristics of deep ore body,especially the deep blind ore body can be accurately presented on the reflection coefficient map.
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