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Geophysical exploration of disseminated and stockwork deposits associated with plutonic intrusive rock: a case study on the eastern flank of Colombia's western cordillera

机译:与深成侵入岩相关的散布和储层沉积物的地球物理勘探:以哥伦比亚西部山脉东部侧面为例

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Disseminated deposits are low-grade, large tonnage deposits which are mainly mined for gold, copper, molybdenum and tin. These deposits are normally associated with intermediate to acid plutonic intrusive rocks and all are characterized by intense, extensive hydrothermal alteration of host rocks Disseminated deposit exploration in the tropics suffers from difficult geological mapping due to dense vegetation, lack of rock outcrops and extensive but variable saprolytic weathering Geophysical exploration of these deposits normally includes magnetic, induced polarization and gamma ray spectrometry surveys . The largest RTP total magnetic field anomaly highs are usually associated with diorite porphyry intrusive bodies . Diorites are usually less magnetic than basaltic rocks; thus when magnetic anomaly highs are related to intrusions they can be explained by basic metals' intensive mineralization (including magnetite) associated with porphyry intrusions Magnetic anomaly gradients regularly help delineate local discontinuities which can be interpreted as local faults and joints that can be mineralized. Gamma ray spectrometry is useful for determining anomalous potassium, uranium and thorium concentration as it can map alteration halos and linear discontinuities Statistical analysis of the data also can determine the intermediate intrusive / extrusive nature of porphyry intrusions Gamma ray spectrometry can help to determine elemental potassium concentration, regardless of the associated potassium mineral species, thereby enabling alteration mapping in a geological setting related to volcanic-associated massive sulphide base metal and gold deposits An induced polarization survey is useful in outlining disseminated sulphide distribution in porphyry deposits related to chargeability anomaly highs. The results of the Quinchia project's geophysical exploration program are discussed.
机译:散布的矿床是低品位,大吨位的矿床,主要开采金,铜,钼和锡。这些矿床通常与中等深度酸性侵入岩有关,并且均以强烈,广泛的主岩热液蚀变为特征。由于茂密的植被,缺乏岩层露头和广泛而可变的腐泥质,在热带地区进行的分布式矿床勘探面临着困难的地质测绘风化这些矿床的地球物理勘探通常包括磁场,感应极化和伽马射线能谱测量。最大的RTP总磁场异常高通常与闪长岩斑岩侵入体有关。闪长岩通常不如玄武岩具有磁性。因此,当磁异常高与侵入有关时,可以用与斑岩侵入有关的基本金属的强烈矿化作用(包括磁铁矿)来解释。磁异常梯度通常有助于描述局部不连续性,这可以解释为局部断层和可矿化的节理。伽玛射线光谱法可用于确定异常的钾,铀和th浓度,因为它可以绘制蚀变晕和线性间断图,对数据进行统计分析也可以确定斑岩侵入岩的中间侵入/挤压性质伽玛射线光谱法可以帮助确定元素钾浓度,而不考虑与之相关的钾矿物种类,从而能够在与火山相关的块状硫化物贱金属和金矿床有关的地质环境中进行蚀变制图。诱导极化勘测有助于概述斑岩矿床中与带电异常高有关的散布硫化物分布。讨论了Quinchia项目的地球物理勘探计划的结果。

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