矿体包含黄铁矿，黄铜矿和闪锌矿。
The ore body consists of pyrite, chalcopyrite and sphalerite.
这有助于确定如何为经济矿体。
矿体你是如何渗透到矿井计划？
可能要求在矿体外作专门钻探或坑探。
品位的急剧下降是矿体边界上的规律。
矿体建模是矿山可视化的重要内容之一。
Ore body modeling is one of the most important contents of mine visualization.
巨大的堆型矿体受第三纪倾陡断层控制。
Large stack deposits are controlled by deeply dipping faults Tertiary age.
利用视电阻率切片图来推演矿体展布形态。
Ore distributed shape was deduced by the apparent resistivity section.
银矿体具厚度大，埋藏浅，易开采的特点。
They are charactered by large thickness, shallow burial and easy mining.
由于矿体小，传统印石采制主要是手工挖掘。
Because of the small mine, usually the ore was excavated by hand.
什么是你的矿体深度？
泥炭植物残体是泥炭和泥炭矿体的主要组分。
Plant residues are the main component of peat and its mineral bodies.
介绍矿体地质、破碎方法、浸铀工艺、以及效果评价。
It introduces ore body geology, crushing method, uranium leaching technology and effectiveness evaluation.
建立了矿体模型、损失贫化动态模型和配矿优化模型。
Establishing the ore body model, the loss impoverishment dynamic model and the ore matching optimization model.
随着采矿的不断进行，地下水对矿体的影响日益明显。
With the progress of the mining, the impact of groundwater on ore body is increasingly obvious.
矿体在时间和空间上与燕山早期岩浆活动有一定关联。
The ore body is related to the Early Yanshanian magmatic activity in time and space.
接触带矿体受接触带控制，具矽卡岩型矿体典型特征。
The contact deposit is controlled by the contact zone, and shows typical features of skarn orebody.
矿体赋存于第四系之下，矿化与构造活动及蚀变密切相关。
The orebody occurred below Quaternary, mineralization is closely related to tectonic activity and alteration.
结果表明：采取一定的措施后，排尾后下部矿体可以回采。
The results show that the deposit can be exploited after taking some measures.
在矿体的许多部位，异离体矿石表明有非常特征性的流动构造。
In many parts of the ore bodies the schlieren ore shows a very characteristic flow structure.
铅矿化不仅具有工业意义，而且可作为寻找锡矿体的指示元素。
Lead mineralization not only possesses industrial significance but is the guide element to find tin orebodise.
冬瓜山矿的矿体埋深大，因而存在高应力，并且各向应力不均衡。
There are high and uneven stresses in the orebody of Dongguashan Mine due to its deep occurrence.
层状主矿体中金主要以细小的自然金形式包裹于斑铜矿和黝铜矿中。
Gold in strati form major orebody is mainly included in bornite and tetrahedrite as fine grain of native gold.
这些模型可对连续矿体的单个或多个采场进行设计并完成经济分析。
These models are capable of designing and performing economic analysis for one or more stopes for a continuous orebody.
在此基础上，分析了拉底参数对矿体崩落系数和底部稳定性的影响。
On that basis, the influence of undercut parameter on the cavability index and opening stability is analysed.
大塘坡原生锰矿矿体形态和矿石结构较复杂，构造简单，属滨海盆地相沉积。
The shape of Datangpo primary manganese deposit and its ore structure are comparatively complex but the structure is simple which belongs to the sedimentary of littoral basin facies.
因此，矿体的原生晕和原生叠加晕特征可指导本区斑岩型铜矿体的成矿预测。
Therefore, the characteristics of primary and primary overprint halo have some guide significance in metallogenic prediction of porphyry copper bodies in this area.
因此，矿体的原生晕和原生叠加晕特征可指导本区斑岩型铜矿体的成矿预测。
Therefore, the characteristics of primary and primary overprint halo have some guide significance in metallogenic prediction of porphyry copper bodies in this area.
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