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    陈树旺. 云开地区断裂构造对金矿的控制作用[J]. 地质与资源, 1994, 3(1): 32-37. DOI: 10.13686/j.cnki.dzyzy.1994.01.003
    引用本文: 陈树旺. 云开地区断裂构造对金矿的控制作用[J]. 地质与资源, 1994, 3(1): 32-37. DOI: 10.13686/j.cnki.dzyzy.1994.01.003
    shu
    Chen Shuwang. THE FAULT CONTROLLING ACTIONS ON THE GOLD DEPOSITS IN YUNKAI AREA[J]. Geology and Resources, 1994, 3(1): 32-37. DOI: 10.13686/j.cnki.dzyzy.1994.01.003
    Citation: Chen Shuwang. THE FAULT CONTROLLING ACTIONS ON THE GOLD DEPOSITS IN YUNKAI AREA[J]. Geology and Resources, 1994, 3(1): 32-37. DOI: 10.13686/j.cnki.dzyzy.1994.01.003
    shu

    云开地区断裂构造对金矿的控制作用

    THE FAULT CONTROLLING ACTIONS ON THE GOLD DEPOSITS IN YUNKAI AREA

      摘要
    • 摘要: 云开地区断裂构造对金矿的控制主要表现在两个方面：其一，断裂带带内的大断裂及大断裂的次级断裂，分别控制着区内的金矿带、矿带内的主要金矿床（点）及金矿体；其二，断裂构造的力学性质、活动期次及构造岩发育程度等，控制或影响着金矿的矿石组构特征、矿化期次及矿化强度等。本文还对断裂构造的控矿机制进行了探讨。

       

      Abstract: The fault controlled the forming of the gold deposits in Yunkai area,mainly shows asfollow: one is the fault zone,the macro-fault and the secondary fault contrelled the occur-rences of the gold mineralization,gold deposits(ore spots)and the ore-bodies respectivelyin the zone.The other is the mechanical property,stage and strength of the fault,they con-trolled or influenced the ore texture,the mineralization stage and the mineralization intensityect.In addition,the author study on ore-control mechanism of the fault.

       

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