甘肃成县庙沟铅锌矿成矿环境及控矿构造分析
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摘要
甘肃成县庙沟铅锌矿床位于秦岭造山带西部,西(和)-成(县)铅锌矿田东段,矿床类型属喷流沉积型。岩石、矿石微量元素特征表明矿区形成时为贫氧环境;稀土元素Eu异常特征反映矿区古成矿流体温度较低,与厂坝-李家沟铅锌矿床形成条件相似; Ce异常特征亦反映矿区形成于贫氧的还原环境。通过探矿工程揭露,认为银洞湾矿段受其北东侧断层(F)与南西侧陡倾矿体共同控制,构造挤压是矿区形成高品位矿石的主要原因。结合区域上的研究成果,建立了矿区成矿模式,指出矿区应注意寻找块状、网脉状矿体,赋存于标高1700～1500m空间内的矿体,以及被断层(F)断失的矿体。
The Miaogou lead-zinc deposit is located in the eastern of Xihe-Chengxian lead-zinc ore cluster which belongs to the western of Qinling orogenic belt,belonging to a sedimentary exhalative deposit. The analytical results of trace elements indicate that forming environment of rocks and orebodies were under oxygen-poor condition; the characteristics of Eu anomaly reflect the lower temperature of paleo-mineralized fluids in Miaogou area,which is similar to the formation conditions of the Changba-Lijiagou lead-zinc deposit; the anomalous characteristics of Ce also reflect the the environment of formation was reduction. According to the exploration engineering( tunnels and drillings),it is considered that Yindongwan ore section is jointly controlled by the northeast side fault( F) and steep-dip orebody on the southwest side,and structural compression of intrusive is the main reason for forming high grade ore. Finally,based on regional research achievements,the metallogenic model of the Miaogou area is established. It is pointed out that we should pay attention to finding massive and stockwork orebodies,and the orebodies were hosted in the space of the elevation of 1700-1500 m,and the orebodies were lost by the fault( F).
The Miaogou lead-zinc deposit is located in the eastern of Xihe-Chengxian lead-zinc ore cluster which belongs to the western of Qinling orogenic belt,belonging to a sedimentary exhalative deposit. The analytical results of trace elements indicate that forming environment of rocks and orebodies were under oxygen-poor condition; the characteristics of Eu anomaly reflect the lower temperature of paleo-mineralized fluids in Miaogou area,which is similar to the formation conditions of the Changba-Lijiagou lead-zinc deposit; the anomalous characteristics of Ce also reflect the the environment of formation was reduction. According to the exploration engineering( tunnels and drillings),it is considered that Yindongwan ore section is jointly controlled by the northeast side fault( F) and steep-dip orebody on the southwest side,and structural compression of intrusive is the main reason for forming high grade ore. Finally,based on regional research achievements,the metallogenic model of the Miaogou area is established. It is pointed out that we should pay attention to finding massive and stockwork orebodies,and the orebodies were hosted in the space of the elevation of 1700-1500 m,and the orebodies were lost by the fault( F).
引文
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Guo A'qian,Ding Zhenju,Wen Chengxiong.2011.Zircon U-Pb dating of granite in Xihe-Chengxian lead-zinc ore cluster in Gansu province,and its geological significance[J].Acta Mineralogica Sinica,(Supplement):581-582(in Chinese).
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Hu Qiaoqing,Wang Yitian,Mao Jingwen,Wei Ran,Liu Shengyou,Ye Dejin,Yuan Qunhu,Dou Ping.2015.Timing of the formation of the Changba-Lijiagou Pb-Zn ore deposit,Gansu Province,China:Evidence from Rb-Sr isotopic dating of sulfides[J].Journal of Asian Earth Sciences,103:350-359.
Jones B,Manning D A C.1994.Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones[J].Chemical Geology,111(1-4):111-129.
Kuang Wenlong,Chen Niansheng,Zhang Wanhu,Liu Xinhua,Chen Xinyue,Zhu Wei,Dai Deqiu.2009.Discussion on the minerogenetic process for Changba-Lijiagou SEDEX type lead-zinc deposits[J].Geotectonica et Metallogenia,32(4):542-547(in Chinese with English abstract).
Li Ying.1983.Mineralization mechanism of stratabound lead-zinc ore deposits in Xicheng ore field[J].Geochimica,3:241-249(in Chinese with English abstract).
Li Ying,Qi Sijing,Ma Guoliang,Zhang Zhenfei.1999.Major characteristics and formation conditions of super large sedimentary-hydrothermal sulfide ore deposits in North China[J].Journal of Xi'an Engineering University,21(4):19-24(in Chinese with English abstract).
Li Zongjin,Shi Laohu,Jin Wenqiang.2014.Geological characteristics and genetic analysis of Miaogou lead-zinc deposit[J].Modern Mining,(7):107-108(in Chinese).
Li Zuochen,Pei Xianzhi,Li Ruibao,Pei Lei,Hu Bo,Liu Chengjun,Chen Guochao,Chen Youxin.2013.LA-ICP-MS zircon U-Pb dating,geochemistry of the Mishuling intrusion in western Qinling and their tectonic significance[J].Acta Petrologica Sinica,29(8):2617-2634(in Chinese with English abstract).
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Ma Guoliang,Qi Sijing,Li Ying,Xue Chunji.1996.A study of the exhalative origin of the Changba lead-zinc deposit,Gansu province[J].Contributions to Geology and Mineral Resources Research,11(3):36-44(in Chinese with English abstract).
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