矿化系统具有地幔岩浆系统，渗透性深层断层和含矿性气热热液系统三大系统。
The mineralization system has three giant system, namely mantle magmatic system, penetrability deep-fault and ore-bearing pneumato-hydrothermal system.
沉积型砂岩容矿的铜钴矿床和含钴的岩浆岩型硫化铜镍矿床是两个最重要的钴矿床类型。
The copper-cobalt deposits hosted in the sedimentary sandstone and the cobalt-bearing magmatic Cu-Ni sulphide deposits are two kinds of the most important cobalt deposits.
总结含矿白云岩、富钾板岩和富钠岩石三者之间在成因方面的关系，认为其属于同一岩浆起源的碱性岩系。
The paper concludes genetic relationship between the ore-bearing dolomitite, K-rich slate and Na-rich slate and believes that they are one alkali rock series of comagmatic origin.
本文揭示了火山角砾岩筒形成中侵入凝灰岩化过程的主导作用、火山角砾岩筒参数和含矿性与岩浆活动专属性的关系。
The leading role of tuffisitization processes in formation of diatremes, parameters and ore content of diatremes relation to peculiarities of the magmatism manifestation are revealed.
该系统包括“三大”成矿体系，即：幔源岩浆体系、深穿透断裂构造体系、含矿气液流体体系。
The mineralization system has three giant system, namely mantle magmatic system, penetrability deep-fault and ore- bearing pneumato-hydrothermal system.
构造运动往往伴随有岩浆活动，含矿流体在构造动力和岩浆热力的驱动下产生活化转移。
Tectonic movement sometimes go with magma activity, and make fluid which include ore elements occur activation and transfer with the tectonic dynamic and magma heat.
含矿岩体是同化了壳源组分且经历了充分的岩浆重力分异作用后脉动式侵位的。
It seems quite probable that the ore bearing intrusions were formed by repeated intruding after assimilating crustal materials penetrated and after sufficient gravitational differentiation.
文章从成矿地质条件、矿床地质特征等入手，分析了矿床的控矿因素，认为该矿床受含矿地层、韧脆性剪切带构造、岩浆岩等因素的制约。
Based on ore-forming condition and ore geology, ore-controlling factors are analyzed. It is suggested that the deposit is controlled by ore-hosting strata, ductile-brittle shear zone and magmatism.
文章从成矿地质条件、矿床地质特征等入手，分析了矿床的控矿因素，认为该矿床受含矿地层、韧脆性剪切带构造、岩浆岩等因素的制约。
Based on ore-forming condition and ore geology, ore-controlling factors are analyzed. It is suggested that the deposit is controlled by ore-hosting strata, ductile-brittle shear zone and magmatism.
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