首页> 外文会议>Eighth international heavy minerals conference 2011. >Application of Ground Magnetic Surveys over Heavy Mineral Sand Strands to Increase Confi dence in the Interpreted Continuity of the Modelled Resources
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Application of Ground Magnetic Surveys over Heavy Mineral Sand Strands to Increase Confi dence in the Interpreted Continuity of the Modelled Resources

机译:应用重矿物砂矿上的地磁测量来增加对模拟资源解释连续性的信心

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The suitability of magnetic surveys fl own at low altitudes to identify buried heavy mineral (HM) strandsrnhas long been accepted. This is despite the low intensity magnetic response often obtained from suchrnstrands. The fundamentals of the magnetic survey method dictate that the closer the instrument isrnto the source the stronger the response. As such the optimal elevation for the magnetometer is at orrnnear the surface.rnIluka sought to use a ground based magnetometer to aid in the exploration target generation processrnand allow accurate targeting of exploration drill holes. Following the initial trial Iluka recognisedrnthe potential additional application of data obtained by a ground based magnetometer over knownrnstrand deposits.rnThe detail of the ground magnetic images can confi rm the assumed strand continuity betweenrncross-sections of close spaced drilling and can aid in the defi nition of the geometry of differentrngenerations of mineralisation. The ability to confi dently determine that the deposit has not beenrntruncated by post emplacement erosion of the mineralised deposit may enable reductions in drillingrnrequirements as well as assisting mine planning activities. Iluka intends to investigate advancedrnmodelling of the magnetic data to determine the level of strand geometry and HM content resolutionrnthat can be achieved from the ground magnetic survey data and its potential application in the miningrngrade control process.rnIt is anticipated that the surveying of Iluka’s known resource deposits will provide the ability torncorrelate the magnetic response from new exploration targets with those from known deposits for arngiven depth, HM grade and mineralogy suite.
机译:长期以来,人们一直接受在低海拔地区进行磁性测量以识别埋藏的重矿物(HM)股线的适用性。尽管经常从这样的钢绞线获得低强度的磁响应,但这是不可行的。磁测法的基本原理要求仪器越靠近震源,响应越强。因此,磁力计的最佳标高位于表面附近。rnuka试图使用基于地面的磁力计来辅助勘探目标的生成过程,并允许精确瞄准勘探钻孔。在初步试验之后,Iluka认识到了地面磁强计获得的数据可能会更多地应用于已知的矿床沉积物上。地面磁像的细节可以确认近距离钻探横截面之间假定的钢绞线连续性,并且可以帮助确定矿化世代的几何形状。确信地确定矿床未因矿床的位后侵蚀而被截断的能力可以减少钻井需求,并协助进行矿山规划活动。 Iluka打算对磁数据进行高级建模,以确定可以从地面磁测量数据中获得的钢绞线几何形状和HM含量分辨率rn及其在采矿级控制过程中的潜在应用.rn预计对Iluka已知资源矿床的勘测将提供使新勘探目标的磁响应与已知矿床的已知矿床,HM等级和矿物学套件的磁响应相互关联的功能。

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