胶东三山岛-仓上断裂带控矿规律与找矿勘查实践
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摘要
三山岛-仓上断裂带是我国著名胶东金矿集区重要的金矿成矿带之一;近十年来,地勘单位与科研院校针对该成矿带深部资源的预测与勘查做了大量的工作,并提出了阶梯式成矿模式。三山岛-仓上断裂带断裂带主裂面整体较陡,主要沿不同岩体的接触面进行展布,从上至下整体呈现逐渐变缓的趋势,构造蚀变带纵向上呈"S"型或反"S"型的张裂处为成矿提供了有利空间,区域内金矿体主要赋存在主裂面的下盘。对断裂带宏观和微观地质特征的分析显示,断裂带北部在三山岛地段走向NE以张剪性为主,赋存矿体延深大于延长;而在南部新立地段和仓上地段之间断裂带走向近NEE以张性为主,赋存矿体延长大于延深。针对三山岛-仓上成矿带南部与北部成矿地质条件的差异性,有针对性布设探矿工程,南部布设工程走向间距可大于倾向间距,钻孔相对较浅;北部布设工程倾向间距可大于走向间距,钻孔相对较深。
The Sanshandao-Cangshang fault zone is a major gold metallogenic belt in the famous Jiaodong gold mine,Shandong Province. In recent ten years,geological prospecting units and scientific research institutions have done a lot of work on the prediction and exploration of deep resources in this metallogenic belt,and put forward a model of ladder-type mineralization. The main fracture surface of this fault zone is generally steep,extending along contact surfaces of different rock masses,becoming gradually gentle down from top to bottom. The"S"-type or anti-"S"-type tensile fractures in the longitudinal direction of the tectonic alteration belt provide favorable space for mineralization,and the gold ore bodies in the region mainly occur in the footwall of the main fracture plane. Analysis of the macroscopic and microcosmic geological characteristics of the fault zone indicates that the northern part of the fault zone trends in NE in the Sanshandao section,dominated by the extension and shear,and the vertical extension of the ore body is greater than its horizontal range. In the south,the fault zone between Xinli and Cangshang section strikes nearly in NEE,dominated by extension,and horizontal extension of the orebody is greater than its downward depth. In view of the difference of the metallogenic geological conditions between the south and the north of this metallogenic belt,a prospecting scheme is suggested that shallow boreholes should be drilled in the south with larger survey-line intervals in horizontal direction than vertical direction and deeper boreholes should be drilled in the north with larger survey-line intervals in the vertical direction than horizontal direction.
The Sanshandao-Cangshang fault zone is a major gold metallogenic belt in the famous Jiaodong gold mine,Shandong Province. In recent ten years,geological prospecting units and scientific research institutions have done a lot of work on the prediction and exploration of deep resources in this metallogenic belt,and put forward a model of ladder-type mineralization. The main fracture surface of this fault zone is generally steep,extending along contact surfaces of different rock masses,becoming gradually gentle down from top to bottom. The"S"-type or anti-"S"-type tensile fractures in the longitudinal direction of the tectonic alteration belt provide favorable space for mineralization,and the gold ore bodies in the region mainly occur in the footwall of the main fracture plane. Analysis of the macroscopic and microcosmic geological characteristics of the fault zone indicates that the northern part of the fault zone trends in NE in the Sanshandao section,dominated by the extension and shear,and the vertical extension of the ore body is greater than its horizontal range. In the south,the fault zone between Xinli and Cangshang section strikes nearly in NEE,dominated by extension,and horizontal extension of the orebody is greater than its downward depth. In view of the difference of the metallogenic geological conditions between the south and the north of this metallogenic belt,a prospecting scheme is suggested that shallow boreholes should be drilled in the south with larger survey-line intervals in horizontal direction than vertical direction and deeper boreholes should be drilled in the north with larger survey-line intervals in the vertical direction than horizontal direction.
引文
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Deng Jun,Wang Qingfei,Wan Li,Yang Liqiang,Gong Qingjie,Zhao Jie,Liu Huan.2009.Self-similar fractal analysis of gold mineralization of Dayingge Zhuang disseminated veinlet deposit in Jiaodong gold province,China[J].Journal of Geochemical Exploration,102:95-102.
Deng Jun,Chen Yumin,Liu Qin.2010.The gold metallogenic system and mineral resources exploration of Sanshandao fault zone,Shandong Province[M].Beijing:Geological Publishing House:60-78(in Chinese).
Dong Jian,Chen Lei,Zhang Guili.2018.Characteristics of geophysical fields around gold deposits inthe Xiadian region,Shandong Province[J].Geology and Exploration,54(1):138-147(in Chinese with English abstract).
Fan Hongrui,Hu Fangfang,Yang Jinhui,Shen Kun,Zhai Mingguo.2005.Fluid evolution and large-scale gold metallogeny during Mesozoic tectonic transition in the eastern Shandong Province[J].Acta Petrologica Sinica,21(5):1317-1328(in Chinese with English abstract).
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Li Hongkui,Li Yifan,Geng Ke,Zhuo Chuanyuan,Zhang Yubo,Liang Taitao.2011.Study on the orogenic type gold deposits in eastern Shangdong Province[J].Geotectonica et Metallogenica,35(4):533-542(in Chinese with English abstract).
Li Shixian,Liu Changchun,An Yuhong,Wang Weicong,Huang Tailing,Yang Chengmei.2007.Geology of gold deposits in Jiaodong[M].Beijing:Geological Publishing House:1-423(in Chinese).
Liu Liandeng,Yao Fengliang.1989.Remelted magnetite granites and the associated gold deposits in the northwest part of the Jiaodong Peninsula[J].Journal of Changchun University of Earth Sciences,19(3):241-251(in Chinese with English abstract).
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Miao Laicheng,Zhai Yusheng,Zhu Chengwei,Guan Kang,Luo Zhenkuan.1999.Discussion on the relationship between granitoid intrusives and gold mineralization-A case study on Zhaoye gold belt,East Shandong Province[J].Acta Geoscientia Sinica,20(supp.):332-336(in Chinese with English abstract).
Sun Huashan,Sun Lin,Zhao Xianhui,Yang Kaichun,Cao Xinzhi,Liu Wensheng,Wang Chao.2007.Ore-controlling evidence and ore prospecting significance of Guojialing granodiorite in northwest Jiaodong Peninsula[J].Gold,28(4):14-18(in Chinese with English abstract).
Qiu Yumin,Groves David I,Mc Naughton Neal J,Wang Lianggen,Zhou Taihe.2002.Nature,age,and tectonic setting of granitoid-hosted,orogenic gold deposits of the Jiaodong Peninsula,eastern North China Craton,China[J].Mineralium Deposita,37:283-305.
Song Guozheng,Li Shan,Yan Chunming,Bao Zhongyi,Fan Jiameng,Liu Caijie,Liu Guodong,Guo Zhifeng.2018.Geological characteristics and prospecting direction of No.I main orebody in the Jiaojia gold deposit[J].Geology and Exploration,54(2):219-229(in Chinese with English abstract).
Song Mingchun,Cui Shuxue,Jiang Hongli.2011.Metallogenic structural system for Jiaojia gold field and Jiaoxibei gold deposits concentrated areas in Shandong Province,China[J].Geological Bulletin of China,30(4):573-578(in Chinese with English abstract).
Song Mingchun,Zhang Junjin,Zhang Pijian,Yang Liqiang,Liu Dianhao,Ding Zhengjiang,Song Yingxin.2015.Discovery and tectonicmagmatic background of superlarge gold deposit in offshore of northern Sanshandao,Shandong Peninsula,China[J].Acta Geologica Sinica,89(2):365-383(in Chinese with English abstract).
Sun Jinggui,Hu Shouxi,Ling Hongfei.2000.Study on the geochemistry and subduction-crust mantle interaction of thehigh potassium-potassium dike rocks in gold deposits concentration zone of east Shandong,China[J].Acta Petrologica Sinica,16(3):401-412(in Chinese with English abstract).
Wang Denghong,Lin Wenwei,Yang Jianming,Yan Shenghao.1999.Controlling effects of the mantle plume on the Jiaodong and DianQian-Gui gold-concentration areas[J].Acta Geoscientia Sinica,20(2):157-162(in Chinese with English abstract).
Wang Junting,Sun Zhongfeng.2005.Study on metallogenic regularity and metallogenic prediction of Xinli gold deposit in Laizhou,Shandong province[M].Beijing:Geological Publishing House:14-20(in Chinese).
Xu Jiuhua,Xie Yuling,Han Qi,Li Qianmao.2004.Characteristics of gold bearing sulfides and their geological significance in Sanshandao gold deposit,eastern Shandong Province[J].Geology and Mineral Resources of South China,1:1-6(in Chinese with English abstract).
Yang Kuifeng,Fan Hongrui,Santosh M,Hu Fangfang,Simon A Wilde,Lan Tingguang,Lu Lina,Liu Yongsheng.2012.Reactivation of the Archean lower crust:Implications for zircon geochronology,elemental and Sr-Nd-Hf isotopic geochemistry of late Mesozoic granitoids from northwestern Jiaodong Terrane,the North China Craton[J].Lithos,146-147:112-127.
Yang Kuifeng,Zhu Jituo,Cheng Shenghong,Liu Xuan,Jiang Peng,Fan Hongrui.2017.Structural controls of the Sanshandao gold deposit in the northwestern Jiaodong district,China[J].Geotectonica et Metallogenia,41(2):272-282(in Chinese with English abstract).
Yao Fengliang,Liu Liandeng,Kong Qingcun,Gong Runtan.1983.The stability isotopic geology and the origin of the gold deposit in the Zhaoyuan-Yexian gold belt,Shandong Province[J].Journal of Changchun University of Earth Sciences,(4):7-18(in Chinese with English abstract)
Zhang Liang,Li Guangwei,Zheng Xiaoli,An Ping,Chen Bingyu.2016.40Ar/39Ar and fission-track dating constraints on the tectonothermal history of the world-class Sanshandao gold deposit,Jiaodong Peninsula,eastern China[J].Acta Petrologica Sinica,32(8):2465-2476(in Chinese with English abstract).
Zhai Mingguo,Yang Jinhui,Liu Wenjun.2001.Large clusters of gold deposits and large-scale metal logenesis in the Jiaodong Peninsula,eastern China[J].Science in China(Series D),44:758-768(in Chinese with English abstract).
Zhai Mingguo,Santosh M.2011.The Early Precambrian odyssey of the North China Craton:A synoptic overview[J].Gondwana Research,20:6-25.
Zhao Yue,Zhai Mingguo,Chen Hong,Zhang Shuanhong.2017.PaleozoicEarly Jurassic tectonic evolution of North China Craton and its adjacent orogenic belts[J].Geology in China,44(1):44-60(in Chinese with English abstract).
Zhou Taihe,Lyu Guxian.2000.Tectonics,granitoids and Mesozoic gold deposits in east Shandong,China[J].Ore Geology Reviews,16(1-2):71-90.
陈光远,邵伟,孙岱生.1989.胶东金矿成因矿物学与找矿[M].重庆:重庆出版社:125-234.
程红军,陈川,展新忠,常金雨,丁亚龙,库瓦尼西别克·买买提朱马,杨蕤嘉,加娜尔,付翰泽.2017.隐伏矿床成矿预测理论与方法新进展[J].地质与勘探,53(3):456-453.
邓军,陈玉民,刘钦.2010.胶东三山岛断裂带金矿成矿系统与资源勘查[M].北京:地质出版社:60-78.
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