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Gravity Measurements Reveal Concealed Rock Masses Surrounds Molybdenum Deposit

机译:重力测量显示隐藏的岩体围绕钼矿床

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Daqinggou molybdenum deposit is an important part of the eastem Qinling molybdenum belt which locates in daqinggou miaozi village area,luanchuan county,Henan province.This is also a part of the Huaxiong margin depression in the North China Platform and it is considered to be a favorable metallogenic area because of the intense tectonic movement and frequent magrnatic activities.This molybdenum deposit is a medium-sized deposit and the ore bodies are strictly controlled by stratum,lithology,structures and environment of ancient geography as well as magmatic rocks.The author compares the difference of physical properties in the first place,then divides research area into two abnormal areas (North and South) and identifies four density layers and three interfaces in the vertical direction with bouguer gravity anomaly.Secondly,It is found that there includes two first level and ninety-eight second level faults.Particularly,there are fifty faults toward NW-NWW,forty faults toward NE-NNE,four faults toward EW and the last six faults toward SN.Different types of data processed gravity maps are analyzed and it is clearly seen that sharp contrasts locate in Linear extreme zone from horizontal direction derivative,dislocation interfaces in gravity anomaly curves,Linear gradient belts from bouguer gravity anomaly.According to some geological data and second derivative gravity map,it is also inferred that there are three hidden rock masses in research area which are G5 low density anomaly,G6 low density anomaly and G9 low density anomaly between Caledonian Iron rich ekerite and the location of north Taihua group.Last but not least,Gravity prospecting marks are summarized in this paper.In conclusion,this research plays an important role in selecting prospecting target area in hidden porphyry type polymetallic molybdenum deposit which belongs to eastern Qinling Mountains-Dabie Mountains molybdenum ore belt and providing reliable evidences for the expansion of old molybdenum mine.
机译:大庆沟钼矿床是河南省栾川县大庆沟苗寨村地区的央秦岭钼腰带的重要组成部分。这也是华北平台华兴裕幅萧条的一部分,被认为是一个有利的由于强烈的构造运动和频繁的Magrnatic活性,所以钼沉积物是一种中型沉积物,矿体由古代地理的地层,岩性,结构和环境以及岩石岩体严格控制。作者比较了物理性质的差异首先,将研究区域划分为两个异常区域(南北),并在垂直方向上识别四个密度层和三个接口,与Bouguer Gravity异常。第二个,发现包括两个第一级和九十八秒的级别断裂。朴素化地,朝鲜NW-NWW,对NENNE的四十几个故障,FOU r故障对EW和最后六个故障对SN.进行了分析的类型的数据处理重力图,清楚地看出,从水平方向衍生物,重力异常曲线中的位错接口,线性梯度带的线性极端区域中的锐度对比度。 Bouguer重力异常。根据一些地质数据和第二衍生物重力图,还推断出在Caledonian铁富含Ekerite之间的G5低密度异常,G6低密度异常和G9低密度异常中有三个隐藏的岩体。北太极集团的地点。但并非最不重要的是,在本文中总结了重力勘探标志。在本文中,这项研究在选择属于东秦岭的隐藏斑岩型多金属钼矿床中的勘探目标区域在选择勘探目标区域方面发挥着重要作用 - Dabie Mountains Moldbdenum Ore皮带,为旧钼矿的扩展提供可靠的证据。

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