桂西北矿集区锡多金属矿床成矿规律
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国家深部探测技术与实验研究专项“南岭成矿带地壳岩浆系统结构探测实验研究”(编号Sinoprobe-03-01),中国地质调查局“全国重要矿产区域成矿规律研究”(编号1212011121037)和“中国分矿种(组)矿产地质总结研究”(编号 12120114039601)、“中国矿产地质与区域成矿规律综合研究(中国矿产地质志)”项目(编号1212011220369)、国土资源部公益性行业科研专项“广西大厂锡石硫化物型锡矿科学基地研究”(编号200911007-13)


Metallogenic Regularity of Tin Polymetallic Deposit from Northweatern Ore Concentration Area, Guangxi
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    摘要:

    桂西北矿集区是我国重要的有色金属基地之一,成矿条件好,找矿潜力大、研究程度高。本文概要介绍了矿集区的成矿地质背景和矿产分布。以南丹-昆仑关成矿带为重点,总结了矿床类型、矿化和围岩蚀变分带特征,提出矿田、矿床的产出一方面受NW向构造与NE向构造的交汇隆起部位、背斜核部、NW向断裂和褶皱的拐弯部位、背斜轴部的局部隆起地段等有利构造部位的控制,另一方面也受岩体侵入构造的控制。围绕隐伏花岗岩体,围岩蚀变由内向外表现为云英岩化→矽卡岩化、角岩化→钾长石化、电气石化、硅化、绢云母化、碳酸盐岩化→绢云母、绿泥石化、碳酸盐化;矿化组合表现为高温W-Mo矿化、Zn-Cu-Sn矿化→高中温Sn多金属矿化→中低温Pb-Zn矿化→低温Sb-Hg-As矿化的正向分带特征,中低温的W-Sb矿化叠加于近岩体矽卡岩型Zn-Cu矿化之上,使得晚期成矿表现出逆向分带特征。利用硫、碳、氧同位素组成及其空间变化,探讨了成矿物质运移方向是由近岩体向远离岩体运移,证实了矿集区内矿床的成因为岩浆热液成因。本文依据赋矿围岩的性质、矿体产出的部位、矿体的类型和形态等特征建立了区域成矿模式,直观地反映了成矿带的成矿特征,对指导该地区的找矿实践具有现实的指导意义。

    Abstract:

    Ore concentration area in northwestern Guangxi is one of the important base of nonferrous metals in China,With the good metallogenic conditions, larger ore prospecting potential, high degree research.The paper briefly introduces the geological background and deposit distribution in the ore concentration area.Taking the Nandan-Kunlunguan metallogenic belt is the key,summariaes the deposit types ,the zoning characteristics of wall rock alteration and minwealization.Proposed the output of the ore field and ore deposits, on the one hand,is controlled by the favorable tectonic position ,such as the intersection uplift position of NW and NE tectonic,anticiline core,the turn position of NW fault and fold, the local uplift position of the anticline axis.On the other hand,is controlled by the intrusive tectonic of granite. Surrounding the concealed granite rock,wall rock from inside to outside shows greisenization→skarn,hornfels→feldspathization, tourmalinization, silicification, sericitization, carbonatization→sericite, chlorite, carbonate; mineralization assemblage shows the normal zoning characteristics of high-temperature W-Mo metallization,Zn-Cu-Sn metallization→High-medium temperature Sn polymetallic metallization→Medium -low temperature Pb-Zn metallization→Low temperature Sb-Hg-As metallization.Low temperature W-Sb deposit superimposed on the skarn type Zn-Cu orebodies near the granite body,show the reverse zoning characteristics in the late mineralization.The composition of sulfur, carbon, oxygen isotope and spatial variation rule show that migration direction of ore-forming material is from near to far from granite orebody. It is confirmed that the genesis of deposites in the ore concentration area belong to magmatic hydrothermal origin.Establed metallogenicl model ,based on the properties of ore-bearing rock,the position of orebody output, type and form of ore deposit, reflects directly the metallogenic characteristics of Nandan-Kunlunguan metallogenic belt,which has importantment guiding significance for the regional prospecting practice.

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梁婷,王登红,蔡明海,黑欢,黄惠明,郑阳.2014.桂西北矿集区锡多金属矿床成矿规律[J].地质学报,88(12):2443-2463.
liang ting, Wang Denghong, Cai Minghai, Hei Huan, Huang Huiming, Zheng Yang.2014. Metallogenic Regularity of Tin Polymetallic Deposit from Northweatern Ore Concentration Area, Guangxi[J]. Acta Geologica Sinica,88(12):2443-2463.

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  • 收稿日期:2014-10-11
  • 最后修改日期:2014-11-06
  • 录用日期:2014-11-12
  • 在线发布日期: 2014-12-09
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