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黄金科学技术 ›› 2019, Vol. 27 ›› Issue (6): 791-801.doi: 10.11872/j.issn.1005-2518.2019.06.791

• 矿产勘查与资源评价 •    下一篇

胶东金地球化学背景研究

陈玉民1(),曾庆栋2,3,4(),孙之夫5,王昭坤1,范宏瑞2,3,4,肖风利1,褚少雄2,3   

  1. 1. 山东黄金集团有限公司,山东 济南 250101
    2. 中国科学院地质与地球物理研究所,中国科学院矿产资源研究重点实验室,北京 100029
    3. 中国科学院地球科学研究院,北京 100029
    4. 中国科学院大学地球科学学院,北京 100049
    5. 山东黄金地质矿产勘查有限公司,山东 莱州 261400
  • 收稿日期:2019-08-22 修回日期:2019-10-28 出版日期:2019-12-31 发布日期:2019-12-24
  • 通讯作者: 曾庆栋 E-mail:chenym@sd-gold.com;zengqingdong@mail.iggcas.ac.cn
  • 作者简介:陈玉民(1961-),男,山东淄博人,高级工程师,从事金矿管理、采矿及找矿工作。chenym@sd-gold.com
  • 基金资助:
    国家重点研发计划项目“华北克拉通成矿系统的深部过程与成矿机理”(2016YFC0600100);山东黄金集团有限公司科研(深钻)项目联合资助

Study on Geochemical Background Field of the Gold Deposits in Jiaodong,China

Yumin CHEN1(),Qingdong ZENG2,3,4(),Zhifu SUN5,Zhaokun WANG1,Hongrui FAN2,3,4,Fengli XIAO1,Shaoxiong CHU2,3   

  1. 1. Shandong Gold Group Co. ,Ltd. ,Jinan 250101,Shandong,China
    2. Key Laboratory of Mineral Resources,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,China
    3. Innovation Academy of Earth Science,Chinese Academy of Sciences,Beijing 100029,China
    4. College of Earth Sciences,University of Chinese Academy of Sciences,Beijing 100049,China
    5. Shandong Gold Geology and Mineral Exploration Co. ,Ltd. ,Laizhou 261400,Shandong,China
  • Received:2019-08-22 Revised:2019-10-28 Online:2019-12-31 Published:2019-12-24
  • Contact: Qingdong ZENG E-mail:chenym@sd-gold.com;zengqingdong@mail.iggcas.ac.cn

摘要:

胶东金矿集区形成于早白垩世构造体制转折期,具有大规模爆发成矿特征,是世界上重要的金矿集中区之一。针对胶东金矿集区成矿物质来源这一科学问题,采用Au元素地球化学分析法系统分析该区地表和深钻样品,揭示该区金的地球化学背景特征,为探讨该区Au元素高强度巨量堆积的成矿作用机制提供地球化学场制约。结果显示:地表胶东群变质岩具有中部高(金丰度均值为1.35×10-9)、东部及西部低(金丰度均值分别为0.95×10-9和0.76×10-9)的地球化学背景场特征;深钻岩石样品的金丰度均值均低于大陆地壳克拉克值及华北地台大陆地壳的金丰度平均值,同样显示亏损地球化学背景场特征。因此,在胶东金矿集区存在金的地球化学亏损场,结合矿区内围岩中普遍存在的热液活动迹象,认为胶东群和中生代花岗岩可能为胶东金矿的形成提供了部分成矿物质。

关键词: 地球化学背景场, 金丰度, 物质来源, 金矿集区, 深钻样品, 胶东

Abstract:

Jiaodong gold ore-concentrating area is the third largest gold mining area in the world after the Lande gold mining area in South Africa and Muruntau gold mining area in Uzbekistan,and its proved gold resources exceed 4 500 t.Jiaodong gold ore-concentrating area formed in the Early Cretaceous tectonic regime transition period and has the characteristics of large-scale concentrated mineralization.This area is composed of a lot of super-large,large gold deposits and includes altered rock type,quartz vein type and interlayer fracture zone type gold deposit.The typical altered rock type gold deposits are Sanshandao,Jiaojia,Xincheng,Dayingezhuang,Xiadian and Dongfeng 171 deposits,and so on.The quartz vein type gold deposits include Linglong,Jinqingding and Denggezhuang deposits,and so on.The interlayer fracture zone type gold deposits are represented by the Pengjiakuang gold deposit.These gold deposits are mainly controlled by the regional faults,secondary faults and interlayer slide faults along the northern margin of the Laiyang basin.The gold deposits in Jiaodong mainly occur within the Mesozoic granite,minor whthin Jiaodong Group,Jingshan Group and Mesozoic strata.This paper selects the scientific problem of the source of ore-forming materials,and systematically analyzes the surface and deep-drilling samples sampled from the Jiaodong area by means of Au element geochemical analysis,in order to reveal the geochemical background characteristics of Au element in this area,and provides geochemical field constraints for discussing the metallogenic mechanism of high-intensity massive accumulation of Au element in this area.The results show that the average abundance of Au element (1.10×10-9) of the Jiaodong group is lower than that of Clark value of continental crust (1.21×10-9) and the value of continental crust of North China Platform,which shows the characteristic of gold deficit geochemical field.Moreover,the results also show that the gold geochemical background feild of the Jiaodong group is characterized by higher average Au abundance in the central area (1.35×10-9) and lower average Au abundance in the east and west of the Jiaodong area (0.95×10-9 and 0.76×10-9).The average abundance of Au element in the fresh rock samples of different rock types (Jiaodong Group,0.79×10-9;Mesozoic granites,0.77×10-9;Gabbro,0.63×10-9;Lamprophyre,0.93×10-9;Acidic dykes,0.82×10-9) from the deep drilling holes is lower than that of Clark value of continental crust and the value of continental crust of North China Platform,which also display the characteristic of gold geochemical deficit field.Therefore,there exists an Au element geochemical deficit field in the Jiaodong ore-concentrating area,combined with the evidence of hydrothermal activities in gold ore areas,we think the Jiaodong Group and the Mesozoic granite might partly provide the source of metallogenic materials for the formation of gold deposits in the Jiaodong area.

Key words: geochemical background field, gold abundance, material resource, gold ore-concentrating area, deep drilling, Jiaodong

中图分类号: 

  • P618.51

图1

胶东金矿地质简图及金地球化学采样点位置(据陈玉民等[10]修改)1.第四系;2.元古宙岩石;3.太古宙岩石;4.超高压变质岩石;5.早白垩世火山岩;6.早白垩世花岗岩;7.早白垩世花岗闪长岩;8.晚侏罗世花岗岩;9.晚三叠世花岗岩;10.主要断层;11.蚀变岩型金矿床;12.石英脉型金矿床;13.层间破碎带角砾岩型金矿床;14.采样点及编号;15.三山岛金矿深钻位置"

表1

胶东地区地表样品Au元素地球化学分析结果统计"

岩石类型w(Au)/(×10-9w(Au)最小值/(×10-9w(Au)最大值/(×10-9样品数量/件样品采集地区
胶东群变质岩0.760.471.086胶西北(莱州—招远)
荆山群大理岩0.720.550.92胶西北(莱州—招远)
玲珑花岗岩0.730.431.2641胶西北(莱州—招远)
郭家岭花岗岩0.690.480.957胶西北(莱州—招远)
中基性岩脉0.630.610.643胶西北(莱州—招远)
胶东群变质岩1.350.533.5315胶东中部(栖霞)
胶东群变质岩0.950.721.5812胶东东部(牟乳—文登)
中生代花岗岩1.180.526.3518胶东东部(牟乳—文登)
大陆地壳1.21中国东部
华北地台大陆地壳1.01 207华北地台

表2

胶西北三山岛金矿深钻样品Au元素分析结果统计"

岩性w(Au)/(×10-9w(Au)最小值/(×10-9w(Au)最大值/(×10-9样品数量/件样品采集地区
胶东变质岩0.790.281.8994胶西北三山岛金矿
中生代花岗岩0.770.262.50209胶西北三山岛金矿
蚀变岩152.300.335 520108胶西北三山岛金矿
辉长岩0.630.301.6418胶西北三山岛金矿
煌斑岩0.930.461.8310胶西北三山岛金矿
酸性脉岩0.820.331.4513胶西北三山岛金矿
大陆地壳1.21中国东部
华北地台大陆地壳1.01 207华北地台

图2

三山岛金矿区深钻孔柱状简图及金丰度图1.胶东群变质岩;2.中生代花岗岩;3.煌斑岩;4.辉长岩;5.酸性岩脉;6.蚀变岩;7.地质界线;8.样品散点图"

表3

胶东地区主要岩石、中国东部变质岩和火成岩及华北地台主要变质岩含金丰度"

岩性样品数量/件w(Au)/(×10-9资料来源
胶东群斜长角闪岩1212.17张韫璞等[44]
胶东群斜长角闪岩7024.2杨士望[20]
胶东群斜长角闪岩9163朱奉三[45]
胶东群斜长角闪岩4姚凤良等[46]
胶东群斜长角闪岩455杨敏之等[47]
胶东群黑云变粒岩22.5杨敏之等[47]
胶东群二云片岩412杨敏之等[47]
胶东群变粒岩7170杨敏之等[47]
胶东群斜长角闪岩621杨敏之等[47]
玲珑花岗岩444.5姚风良等[46]
郭家岭花岗岩306.1姚风良等[46]
煌斑岩315姚风良等[46]
荆山群斜长角闪岩10202杨敏之等[47]
荆山群斜长浅粒岩4150杨敏之等[47]
荆山群石榴石大理岩325杨敏之等[47]
荆山群云母条带大理岩391杨敏之等[47]
荆山群云母片岩330杨敏之等[47]
荆山群黑云石英片岩418杨敏之等[47]
华北地台变粒岩3951.0迟清华等[32]
华北地台麻粒岩3171.4迟清华等[32]
华北地台斜长角闪岩3381.2迟清华等[32]

图3

胶西北三山岛矿区深钻(ZK965)围岩中热液活动细脉(a)混合岩化片麻岩中发育石英—方解石脉(125 m深处);(b)玲珑花岗岩中发育石英—绿泥石脉和硅化(1 320.92 m深处);(c)变形玲珑花岗岩中发育石英细脉(1 989.72 m深处);(d)玲珑花岗岩中发育滑石脉(2 150 m深处)"

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