img

QQ群聊

img

官方微信

高级检索

黄金科学技术 ›› 2018, Vol. 26 ›› Issue (4): 406-422.doi: 10.11872/j.issn.1005-2518.2018.04.406

• • 上一篇    下一篇

胶东金矿床:基本特征和主要争议

宋明春1(),宋英昕2,丁正江3,李世勇4   

  1. 1山东省地质矿产勘查开发局,山东 济南 250013
    2山东省地质科学研究院,山东 济南 250013
    3山东省第八地质矿产勘查院,山东 日照 276826
    4山东省物化探勘查院,山东 济南 250013
  • 收稿日期:2018-03-06 修回日期:2018-04-16 出版日期:2018-10-10 发布日期:2018-10-17
  • 作者简介:宋明春(1963-),男,山东莱阳人,研究员,从事矿产勘查、区域地质调查和相关研究工作。mingchuns@163.com
  • 基金资助:
    山东省重点研发计划项目“深部金矿成矿资源评价理论、方法与预测”(2017CXGC1604);山东省泰山学者建设工程专项经费“胶东型金矿的构造岩浆背景和深部找矿关键技术”(ts201511076)

Jiaodong Gold Deposits:Essential Characteristics and Major Controversy

Mingchun SONG1(),Yingxin SONG2,Zhengjiang DING3,Shiyong LI4   

  1. 1Bureau of Geology and Mineral Resources of Shandong Province,Jinan 250013,Shandong,China
    2Institute of Geological Sciences of Shandong Province,Jinan 250013,Shandong,China
    3Survey Institute of Geology & Mineral Resources of Shandong,Yantai 264003,Shandong,China
    4Shandong Institute of Geophysical and Geochemical Exploration,Jinan 250013,Shandong,China
  • Received:2018-03-06 Revised:2018-04-16 Online:2018-10-10 Published:2018-10-17

摘要:

胶东地区的金矿找矿不断取得新突破,已成为世界第三大金矿集区。本文系统总结了胶东金矿床的空间分布、构造控矿和矿化蚀变等基本特征,分析了存在的主要争议问题。总结指出,胶东金矿床分布于胶西北、栖蓬福和牟乳3个金矿床集中区,有三山岛、焦家、招平、西林—陡崖和金牛山5条主要控矿断裂带。赋矿地质体主要为侏罗纪玲珑型花岗岩、白垩纪郭家岭型花岗岩和新太古代—古元古代变质岩系,白垩纪莱阳群底部也赋存少量金矿床。主要金矿化类型为破碎带蚀变岩型,其次为石英脉型和硫化物石英脉型,有少量金矿化被划分为蚀变砾岩型、盆缘断裂角砾岩型、破碎带石英网脉带型、层间滑动构造带型和黄铁矿碳酸盐脉型,金属量在20 t以上的大型金矿大部分为破碎带蚀变岩型。中型以上金矿床的矿石量加权平均品位为4.07×10-6。胶东金矿床主要受区域性较大断裂及其次级断裂控制,控矿构造型式或位置主要有:断裂的拐弯部位、断裂倾角变化部位、断裂交会部位、入字型构造组合、帚状构造组合、菱形结环状构造组合和雁列构造组合,不同构造控制的金矿体的侧伏方向大致沿SW-NE同一直线方向展布。金矿床的蚀变、矿化、构造具有较好的分带性,破碎带蚀变岩型金矿的分带由弱至强表现为:网脉状—脉状钾化岩带、浸染状—网脉状黄铁绢英岩化碎裂岩化岩带和浸染状黄铁绢英岩质碎裂岩带(或黄铁绢英岩带)。前人虽然对胶东金矿进行了大量研究,但仍然存在一些尚待解决的关键问题,主要争议包括:(1)关于胶东金矿类型的认识主要有岩浆热液型、胶东型、克拉通破坏型和造山型等。(2)关于成矿地质体及成矿物质和流体来源的认识主要有:玲珑花岗岩或郭家岭花岗岩在金成矿中起到了重要作用或者是金矿的成矿地质体,成矿流体源于初始岩浆水;成矿物质来源具有多元性和复杂性,源自中生代活化再造的前寒武纪增生变质杂岩,成矿流体为壳—幔混合来源,以壳源变质流体为主;地幔来源的煌斑岩与金矿化有成因联系,成矿流体可能来源于基性幔源岩浆脱水;胶东金矿的形成与伟德山型花岗岩及同期的脉岩、火山岩有关。(3)关于胶东金矿成矿时代的主要认识有:金矿同位素年龄范围为123.0~110.6 Ma,大多数金矿床形成于(120±5)Ma;或是认为金矿床主要形成于134~126 Ma、122~119 Ma和110~107 Ma 3个时段;有125~115 Ma和100~90 Ma 2期成矿。

关键词: 胶东金矿床, 空间分布, 构造控矿, 金矿类型, 成矿地质体, 物质来源, 成矿时代

Abstract:

Jiaodong has become the third largest gold ore concentration area in the world because of the break-through of gold exploration in recently.This basic characteristics of the spatial distribution,structural ore-controlling,mineralization and alteration of Jiaodong gold deposits were summarized,and the main controversial issues about the gold deposits were analyzed.Jiaodong gold deposits are distributed among the three metallogenetic sub-regions namely the Jiaoxibei,Qipengfu and Muru,and there are five main ore-controlling fault zones. The ore hosting geological bodies in the area are mainly Jurassic Linglong-type granitoid,followed by the early Cambrian metamorphic rocks and the Cretaceous Guojialing-type granitoid,and a small number of gold deposits occurred in the Cretaceous Laiyang group.The major types of gold minralization are altered-rock type in the fracture zone and gold-bearing quartz vein type,and next are braided quartz vein type along the fracture zones,quartz-sulphide vein type,interlayer type along the detachment belt,altered-conglomerate type,breccia type along the basin margin faults and carbonate vein type.The large-sized gold deposits are mostly altered-rock type,and the average grade of the medium and large-sized gold deposits is 4.07×10-6. Jiaodong gold deposits are strictly controlled by regional larger fault and its secondary fault.The ore-controlling tectonic pattern or position mainly include:turn around of the fracture,change parts of fracture angle,intersection part of multi-faults,intersect as small angle of faults,brush structures,the diamond ring structure combination,and echelon structure combination.The long-axis direction of oblique-arrange of gold orebodies that controlled by different fractures are distribution roughly the same straight line along the SW-NE direction.The gold deposits present the zoning characteristics of structure,alternation and mineralization,including cataclasitic zone of pyrite-sericite-quartz alteration,cataclasitic granitoid zone of pyrite-sericite-quartz alteration and potassic granitoid zone.The hydrothermal alteration minerals related to gold mineralization mainly include quartz,sericite,pyrite,chalcopyrite,galena,sphalerite,silver gold and natural gold.Though significant research has been conducted about Jiaodong gold deposits,there are the following key issues remain to be solved.(1)There are magmatic hydrothermal type,Jiaodong type,Cratonic destruction type or orogenic type for the understandings of the Jiaodong gold mineralization.(2)The understandings about the ore-forming geological bodies,the source of ore-forming material and fluid mainly include:Linglong type or Guojialing type granitoid played an important role in mineralization,and ore-forming fluid is the result of initial magmatic water;The ore-forming materials are diversity and complexity that derived from the Precambrian metamorphic basement rock mass which reactivated in the Mesozoic,and ore-forming fluids came from both the crust and mantle and are mainly the crust source metamorphic fluid;Mantle-derived lamprophyre associated with gold mineralization,and ore-forming fluid may be derived from the magma water that formed by the dehydration of the mantle-derived basic magma;The formation of Jiaodong gold deposits is related to the Weideshan type granitoid and its related dikes and volcanics.(3)The understandings about the metallogenic epoch of Jiaodong gold deposits are three main arguments:The isotopic age range is 123.0~110.6 Ma,and mostly are formed at (120±5)Ma;Jiaodong gold deposits formed in three period between 134 and 107 Ma;There are two metallogenic periods at 125~115 Ma and 100~90 Ma.

Key words: Jiaodong gold deposits, spatial distribution, structural ore-controlling, type of gold mineralization, metallogenic geological body, material source, metallogenetic epoch

中图分类号: 

  • P618.51

图1

胶东半岛区域地质和金矿分布简图(据文献[5]修改) ME1-胶西北成矿小区;ME2-栖蓬福成矿小区;ME3-牟乳成矿小区;F1-三山岛断裂;F2-焦家断裂;F3-招平断裂;F4-西林—陡崖断裂;F5-金牛山断裂;1.第四系;2.白垩系;3.古元古界和新元古界;4.含榴辉岩的新元古代花岗质片麻岩;5.太古宙花岗—绿岩带;6.白垩纪崂山型花岗岩;7.白垩纪伟德山型花岗岩;8.白垩纪郭家岭型花岗岩;9.侏罗纪花岗岩类;10.三叠纪花岗岩类;11.整合/不整合地质界限;12.断层;13.以往探明的浅部金矿床位置(图中金矿符号大小依次代表资源储量≥100 t的超大型金矿床、20 t≤资源储量<100 t的大型金矿床、5 t≤资源储量<20 t的中型金矿床和资源储量<5 t的小型金矿床);14.新探明的深部金矿床位置(金矿符号大小含义同图例13);15.蚀变岩型和网脉型金矿,石英脉型和硫化物石英脉型金矿,以及蚀变角砾岩型、蚀变砾岩型和层间滑脱拆离带型金矿"

图2

胶东不同赋矿地质体中所含金矿床数量比例"

图3

胶东金矿床资源量统计"

图4

胶东金矿床的吨位—品位投影图"

图5

焦家断裂构造—蚀变—矿化网络结构"

图6

焦家断裂中段巨型金矿床主要矿体垂直纵投影图"

表1

蚀变岩型金矿构造—蚀变—矿化分带[30]"

分带类型 分带标志 分带特征及变化
构造分带 距主断面距离
构造岩 断层泥 碎裂岩 花岗质碎裂岩 碎裂花岗岩 花岗岩
构造强度 极强 较强 较弱
容矿裂隙 连续弥散空间 连续自由空间
微构造 劈理 平等裂隙 交叉裂隙 张裂隙
蚀变分带 岩石类型 (黄铁)绢英岩 (黄铁)绢英岩化花岗质碎裂岩 (黄铁)绢英岩化碎裂花岗岩 钾化花岗岩
蚀变类型 绢英岩化、黄铁矿化、碳酸盐化 绢英岩化、硅化、黄铁矿化、碳酸盐化 绢英岩化、硅化、黄铁矿化、钾化、碳酸盐化 硅化、钾化、红化
蚀变强度 较强 较弱
矿化分带 成矿方式 交代 充填
矿化类型 稠密浸染状 浸染状、网脉状 网脉状、脉状 脉状
矿石类型 蚀变岩型 蚀变岩型、复合型 复合型、石英脉型 蚀变岩型
矿石组构 碎裂、糜棱、交代结构、浸染状、斑杂状构造 碎裂、花岗变晶结构,浸染状、细脉网脉状构造 碎裂、花岗结构,细脉网脉状构造 晶粒状结构,块状、浸染状构造
矿化强度 较强 较弱

图7

胶东金矿同位素年龄统计(数据来源于文献[63-70])"

1 邓军,徐守礼,方云,等.胶东西北部构造体系及金成矿动力学[M].北京:地质出版社,1996:37-39.
Deng Jun , Xu Shouli , Fang Yun ,et al.Tectonic System in Northwestern Jiaodong Peninsula and Metallogenic Dynamics of Gold[M].Beijing:Geological Publishing House,1996:37-39.
2 李士先,刘长春,安郁宏,等.胶东金矿地质[M].北京:地质出版社,2007.
Li Shixian , Liu Changchun , An Yuhong ,et al.Geology of Gold Deposits in Shandong Peninsula[M].Beijing:Geological Publishing House,2007.
3 吕古贤,孔庆存.胶东玲珑—焦家式金矿地质[M].北京:科学出版社,1993.
Lü Guxian , Kong Qingcun .Geology on the Linglong-Jiaojia-type Gold Deposits in the Jiaodong Area,China[M].Beijing:Science Press,1993.
4 宋明春,崔书学,伊丕厚,等.山东省胶西北金矿集中区深部大型—超大型金矿找矿与成矿模式[M].北京:地质出版社,2010
Song Mingchun , Cui Shuxue , Yi Pihou ,et al.Prospecting and Metallogenic Model of Large and Ultra-large Scale Gold Deposits in Jiaoxibei Ore Concentration Area,Shandong Province[M].Beijing:Science Press,2010.
5 宋明春.胶东金矿深部找矿主要成果和关键理论技术进展[J].地质通报,2015,34(9):1758-1771.
Song Mingchun .The main achievements and key theory and methods of deep seated prospecting in the Jiaodong gold-concentrated area,Shandong Province[J].Geological Bulletin of China,2015,34(9):1758-1771.
6 刘建辉,刘福来,刘平华,等.胶北早前寒武纪变质基底多期岩浆—变质热事件:来自TTG片麻岩和花岗质片麻岩中锆石U-Pb定年的证据[J].岩石学报,2011,27(4):943-960.
Liu Jianhui , Liu Fulai , Liu Pinghua ,et al.Polyphase magmatic and metamorphic events from Early Precambrian metamorphic basement in Jiaobei area:Evidences from the zircon U-Pb dating of TTG and granitic gneisses[J].Acta Petrologica Sinica,2011,27(4):943-960.
7 Liu J H , Liu F L , Ding Z J ,et al.The growth,reworking and metamorphism of early Precambrian crust in the Jiaobei terrane,the North China Craton:Constraints from U-Th-Pb and Lu-Hf isotopic systematics,and REE concentrations of zircon from Archean granitoid gneisses[J].Precambrian Research,2013,224:287-303.
8 颉颃强,万渝生,王世进,等.胶东谭格庄地区奥长花岗质片麻岩和斜长角闪岩的野外地质和锆石SHRIMP定年[J].岩石学报,2013,29(2):619-629.
Xie Hangqiang , Wan Yusheng , Wang Shijin ,et al.Geology and zircon dating of trondhjemitic gneiss and amphibolite in the Tangezhuang area,eastern Shandong[J].Acta Petrologica Sinica,2013,29(2):619-629.
9 Li S Z , Zhao G C , Santosh M ,et al.Paleoproterozoic structural evolution of the southern segment of the Jiao-Liao-Ji Belt,North China Craton[J].Precambrian Research,2012,200/201/202/203(4):59-73.
10 李向辉,陈福坤,李潮峰,等.苏鲁造山带荣成超高压地体片麻岩锆石年龄和铪同位素组成特征[J].岩石学报,2007,23(2):351-368.
Li Xianghui , Chen Fukun , Li Chaofeng ,et al.Zircon ages and Hf isotopic composition of gneisses from the Rong-cheng ultrahigh-pressure terrain in the Sulu orogenic belt[J].Acta Petrologica Sinica,2007,23(2):351-368.
11 唐俊,郑永飞,吴元保,等.胶东地块东部变质岩锆石U-Pb定年和氧同位素研究[J].岩石学报,2004,20(5):1039-1062.
Tang Jun , Zheng Yongfei , Wu Yuanbao ,et al.Zircon U-Pb ages and oxygen isotopes of high-grade metamorphic rocks in the eastern part of the Shandong Peninsula[J].Acta Petrologica Sinica,2004,20(5):1039-1062.
12 匡永生,庞崇进,罗震宇,等.胶东青山群基性火山岩的Ar-Ar年代学和地球化学特征:对华北克拉通破坏过程的启示[J].岩石学报,2012,28(4):1073-1091.
Kuang Yongsheng , Pang Chongjin , Luo Zhenyu ,et al.40Ar-39Ar geochronology and geochemistry of mafic rocks from Qingshan Group,Jiaodong area:Implications for the destruction of the North China Craton[J].Acta Petrologica Sinica,2012,28(4):1073-1091.
13 Ling W L , Xie X J , Liu X M ,et al.Zircon U-Pb dating on the Mesozoic volcanic suite from the Qingshan Group stratotype section in eastern Shandong Province and its tectonic significance[J].Science China:Earth Sciences,2007,50(6):813-824.
14 Liu S , Hu R Z , Gao S ,et al.Zircon U-Pb age,geochemistry and Sr-Nd-Pb isotopic compositions of adakitic volcanicrocks from Jiaodong,Shandong Province,Eastern China:Constraints on petrogenesis andimplications[J].Journal of Asian Earth Sciences,2009,35(5):445-458.
15 邱检生,王德滋,罗清华,等.鲁东胶莱盆地青山组火山岩的39Ar-40Ar定年——以分岭山火山机构为例[J].高校地质学报,2001,7(3):351-355.
Qiu Jiansheng , Wang Dezi , Luo Qinghua ,et al.39Ar-40Ar dating for volcanic rocks of Qingshan formation in Jiaolai basin,eastern Shandong Province:A case study of the Fenlingshan volcanic apparatus in Wulian county[J].Geological Jourrnal of China Universities,2001,7(3):351-355.
16 张岳桥,李金良,张田,等.胶莱盆地及其邻区白垩纪—古新世沉积构造演化历史及其区域动力学意义[J].地质学报,2008,82(9):1229-1257.
Zhang Yueqiao , Li Jinliang , Zhang Tian ,et al.Cretaceous to Paleocene tectono-sedimentary evolution of the Jiaolai basin and the contiguous areas of the Shandong Peninsula (North China)and its geodynamic implications[J].Acta Geologica Sinica,2008,82(9):1229-1257.
17 宋明春,李三忠,伊丕厚,等.中国胶东焦家式金矿类型及其成矿理论[J].吉林大学学报 (地球科学版),2014,44(1):87-104.
Song Mingchun , Li Sanzhong , Yi Pihou ,et al.Classification and metallogenic theory of the Jiaojia-style gold deposit in Jiaodong Peninsula,China[J].Journal of Jilin University (Earth Science Edition),2014,44(1):87-104.
18 王世进,万渝生,郭瑞朋,等.鲁东地区玲珑型(超单元)花岗岩的锆石SHRIMP定年[J].山东国土资源,2011,27(4):1-7.
Wang Shijin , Wan Yusheng , Guo Ruipeng ,et al.SHRIMP zircon dating of Linglong type (superunit)granite in eastern Shandong Province[J].Shandong Land and Resources,2011,27(4):1-7.
19 关康,罗镇宽,苗来成,等.胶东招掖郭家岭型花岗岩锆石SHRIMP年代学研究[J].地质科学,1998,33(3):318-328.
Guan Kang , Luo Zhenkuan , Miao Laichen ,et al.SHRIMP in zircon chronology for Guojialing suite granite in Jiaodong Zhaoye district[J].Scientia Geologica Sinica,1998,33(3):318-328.
20 张田,张岳桥.胶北隆起晚中生代构造—岩浆演化历史[J].地质学报,2008,82(9):1210-1228.
Zhang Tian , Zhang Yueqiao .Late Mesozoic tectono-magmatic evolution history of the Jiaobei uplift,Shandong Peninsula[J].Acta Geologica Sinica,2008,82(9):1210-1228.
21 宋英昕,宋明春,丁正江,等.胶东金矿集区深部找矿重要进展及成矿特征[J].黄金科学技术,2017,25(3):4-18.
Song Yingxin , Song Mingchun , Ding Zhengjiang ,et al.Major advances on deep prospecting in Jiaodong gold ore cluster and its metallogenic characteristics[J].Gold Science and Technology,2017,25(3):4-18.
22 李国华,丁正江,纪攀,等.胶菜盆地东北缘地区金矿特征及找矿方向[J].地质与勘探,2016,52(6):1029-1036.
Li Guohua , Ding Zhengjiang , Ji Pan ,et al.Features and prospecting direction of the gold deposits in the northeastern margin of the Jiaolai Basin[J].Geology and Exploration,2016,52(6):1029-1036.
23 王志新,焦秀美,丁正江,等.胶莱盆地东北缘辽上式金矿构造控矿特征及找矿方向[J].黄金科学技术,2017,25(3):61-69.
Wang Zhixin , Jiao Xiumei , Ding Zhengjiang ,et al.Feature of ore-controlling structure and prospecting direction for the Liaoshang-type gold deposit in the northeast margin of Jiaolai basin,Shandong Province[J].Gold Science and Technology,2017,25(3):61-69.
24 李宏骥.胶北地区内生金矿成矿规律[J].山东地质,2002,18(3/4):72-77.
Li Hongji .Ore-forming rule of endogenetic gold deposit in north of Jiaodong area[J].Geology of Shandong,2002,18(3/4):72-77.
25 Song M C , Deng J , Yi P H ,et al.The kiloton class Jiaojia gold deposit in eastern Shandong Province and its genesis[J].Acta Geologica Sinica,2014,88(3):801-824.
26 宋明春,张军进,张丕建,等.胶东三山岛北部海域超大型金矿床的发现及其构造—岩浆背景[J].地质学报,2015,89(2):365-383.
Song Mingchun , Zhang Junjin , Zhang Pijian ,et al.Discovery and tectonic-magmatic background of superlarge gold deposit in offshore of northern Sanshandao,Shandong Peninsula,China[J].Acta Geologica Sinica,2015,89(2):365-383.
27 沈远超,李厚民,刘铁兵,等.胶西北焦家式金矿化类型及其研究意义[J].地质与勘探,2001,37(1):48-51.
Shen Yuanchao , Li Houmin , Liu Tiebing ,et al.Types of gold mineralization of Jiaojia type’s gold deposits in Jiaodong district,Shandong Province,and their importance of studying[J].Geology and Prospecting,2001,37(1):48-51.
28 邓军.山东招掖金矿带断裂构造分带与蚀变矿化分带关系研究[J].矿床地质,1994,13(增):17-19.
Deng Jun .Relationship between structure,alteration and mineralization zonation in Zhaoye gold metallogenic belt,Shandong Province[J].Mineral Deposits,1994,13(Supp.):17-19.
29 张炳林,杨立强,黄锁英,等.胶东焦家金矿床热液蚀变作用[J].岩石学报,2014,30(9):2533-2545.
Zhang Binglin , Yang Liqiang , Huang Suoying ,et al.Hydrothermal alteration in the Jiaojia gold deposit,Jiaodong,China[J].Acta Petrologica Sinica,2014,30(9):2533-2545.
30 张丕建,宋明春,刘殿浩,等.胶东玲珑金矿田171号脉深部金矿床特征及构造控矿作用[J].矿床地质,2015,34(5):855-873.
Zhang Pijian , Song Mingchun , Liu Dianhao ,et al.Features of deep-seated gold orebodies of No.171 lode and structural ore-controlling action in Linglong gold orefield,Shandong Peninsula[J].Mineral Deposits,2015,34(5):855-873.
31 沈保丰,毛德宝,李俊建.中国绿岩带型金矿床类型和地质特征[J].前寒武纪研究进展,1997,20(4):1-12.
Shen Baofeng , Mao Debao , Li Junjian .Type and geological character of Chinese greenstone belts gold deposits[J].Progress in Precambrian Research,1997,20(4):1-12.
32 杨敏之,吕古贤.胶东绿岩带金矿地质地球化学[M].北京:地质出版社,1996.
Yang Minzhi , Lü Guxian .The Geochemical Characteristic of Gold Deposits in Jiaodong Greenstone Belt[M].Beijing:Geological Publishing House,1996.
33 朱奉三.混合岩化热液金矿床成矿作用初步研究——以招掖地区的金矿床为例[J].地质与勘探,1980(7):1-10.
Zhu Fengsan .Preliminary study on metallogenesis of migmatitic-hydrothermal gold deposits:Taking gold deposits in Zhaoye area as an example[J].Geology and Prospecting,1980(7):1-10.
34 吕古贤,李洪奎,丁正江,等.胶东地区“岩浆核杂岩”隆起—拆离带岩浆期后热液蚀变成矿[J].现代地质,2016,30(2):247-262.
Lü Guxian , Li Hongkui , Ding Zhengjiang ,et al.Hydrothermal alteration metallogenesis in the determination zone of a“magmatic core complex” upheaval-detachment structure,Jiaodong[J].Geoscience,2016,30(2):247-262.
35 杨立强,邓军,王中亮,等.胶东中生代金成矿系统[J].岩石学报,2014,30(9):2447-2467.
Yang Liqiang , Deng Jun , Wang Zhongliang ,et al.Mesozoic gold metallogenic system of the Jiaodong gold province,eastern China[J].Acta Petrologica Sinica,2014,30(9):2447-2467.
36 毛景文,李厚民,王义天,等.地幔流体参与胶东金矿成矿作用的氢氧碳硫同位素证据[J].地质学报,2005,79(6):839-857.
Mao Jingwen , Li Houmin , Wang Yitian ,et al.The relationship between mantle-derived fluid and gold ore-formation in the eastern Shandong Peninsula:Evidences from D-O-C-H isotopes[J].Acta Geologica Sinica,2005,79(6):839-857.
37 孙丰月,石准立,冯本智.胶东金矿地质及幔源C-H-O流体分异成岩成矿[M].长春:吉林人民出版社,1995.
Sun Fengyue , Shi Zhunli , Feng Benzhi .Geological Characteristics,Diagenesis and Mineralization of Gold Deposits Resulting from Differentiation of C-H-O Fluid Derived from Mantle in Jiaodong Peninsula[M].Changchun:Jilin People's Publishing House,1995.
38 陈衍景, Franco P ,赖勇,等.胶东矿集区大规模成矿时间和构造环境[J].岩石学报,2004,20(4):907-922.
Chen Yanjin , Franco Pirajno , Lai Yong ,et al.Metallogenic Time and Tectonic Setting of The JiaodongGoldProvinceEastern China[J].Acta Petrologica Sinica,2004,20(4):907-922.
39 Goldfarb R J , Groves D I , Gardoll S. Orogenic gold and geologic time:A global synthesis[J].Ore Geology Reviews,2001,18(1):1-75.
40 Qiu Y M , Groves D I , McNaughton N G ,et al.Nature,age and tectonic setting of granitoid-hosted,orogenic gold deposits of the Jiaodong Peninsula,eastern North China Craton,China[J].Mineralium Deposita,2002,37(3/4):283-305.
41 Zhou T H , Lu G. Tectonics,granitoids and mesozoic gold deposits in East Shandong,China[J].Ore Geology Reviews,2000,16(1/2):71-90.
42 翟明国,范宏瑞,杨进辉,等.非造山带型金矿——胶东型金矿的陆内成矿作用[J].地学前缘,2004,11(1):85-98.
Zhai Mingguo , Fan Hongrui , Yang Jinhui ,et al.Large-scale cluster of gold deposits in east Shandong:Anorogenic metallogenesis[J].Earth Science Frontiers,2004,11(1):85-98.
43 Goldfarb R J , Santosh M. The dilemma of the Jiaodong gold deposits:Are they unique?[J].Geoscience Frontiers,2014,5(2):139-153.
44 Groves D I , Santosh M. The giant Jiaodong gold province:The key to a unified model for orogenic gold deposits?[J].Geoscience Frontiers,2016,7(3):409-417.
45 Zhu R X , Fan H R , Li J W ,et al.Decratonic gold deposits[J].Science China:Earth Sciences,2015,58(9):1523-1537.
46 Li L , Santosh M , Li S R .The ‘Jiaodong type’ gold deposits:Characteristics,origin and prospecting[J].Ore Geology Reviews,2015,65:589-611.
47 李俊建,罗镇宽,刘晓阳,等.胶东中生代花岗岩及大型—超大型金矿床形成的地球动力学环境[J].矿床地质,2005,24(4):361-372.
Li Junjian , Luo Zhenkuan , Liu Xiaoyang ,et al.Geodynamic setting for formation of large-superlarge gold deposits and Mesozoic granites in Jiaodong area[J].Mineral Deposits,2005,24(4):361-372.
48 罗贤冬,杨晓勇,段留安,等.胶北地块与金成矿有关的郭家岭岩体和上庄岩体年代学及地球化学研究[J].地质学报,2014,88(10):1874-1888.
Luo Xiandong , Yang Xiaoyong , Duan Liu’an ,et al.Geochemical and geochronological study of the gold-related Guojialing pluton and Shangzhuang pluton in Jiaobei block[J].Acta Geologica Sinica,2014,88(10):1874-1888.
49 Wang L G , Qiu Y M , McNaughton N J ,et al.Constraints on crustal evolution and gold metallogeny in the northwestern Jiaodong Peninsula,China,from SHIMP U-Pb zircon studies of granitoids[J].Ore Geology Reviews,1998,13(1/2/3/4/5):275-291.
50 Fan H R , Zhai M G , Xie Y H ,et al.Ore-forming fluids associated with granite-hosted gold mineralization at the Sanshandao deposit,Jiaodong gold province,China[J].Mineralium Deposita,2003,38(6):739-750.
51 姜晓辉,范宏瑞,胡芳芳,等.胶东三山岛金矿中深部成矿流体对比及矿床成因[J].岩石学报,2011,27(5):1327-1340.
Jiang Xiaohui , Fan Hongrui , Hu Fangfang ,et al.Comparative studies on fluid inclusion in different depths and ore genesis of the Sanshandao gold deposit,Jiaodong Peninsula[J].Acta Petrologica Sinica,2011,27(5):1327-1340.
52 刘辅臣,卢作祥,范永香,等.玲珑金矿中基性脉岩与矿化的关系讨论[J].地球科学,1984(4):39-45.
Liu Fuchen , Lu Zuoxiang , Fan Yongxiang ,et al.On the relation between intermediate-basic dykes and mineralization in Linglong gold ore field[J].Earth Science,1984(4):39-45.
53 罗振宽,关康,苗来成.胶东玲珑金矿田煌斑岩脉与成矿关系的讨论[J].黄金地质,2001,7(4):15-21.
Luo Zhenkuan , Guan Kang , Miao Laicheng .Discussion on relationship between lamprophyre veins and mineralization in the Linglong gold field,eastern Shandong[J].Gold Geology,2001,7(4):15-21.
54 孙景贵,胡受奚,凌洪飞,等.胶西北两类金矿田的高钾—钾质脉岩元素地球化学与成岩作用研究[J].地球化学,2000,29(2):143-152.
Sun Jinggui , Hu Shouxi , Ling Hongfei ,et al.Eiembent geochemistry and origin of high potassic-potassic dike rocks in two types of goldfields in Northwest Jiaodong,Shandong,China[J].Geochimica,2000,29(2):143-152.
55 Li S R , Santosh M. Metallogeny and craton destruction:Records from the North China Craton[J].Ore Geology Reviews,2014,56(1):376-414.
56 Shen J F , Li S R , Santosh M ,et al.He-Ar isotope geochemistry of iron and gold deposits reveals heterogeneous lithospheric destruction in the North China Craton[J].Journal of Asian Earth Sciences,2013,78(12):237-247.
57 范宏瑞,胡芳芳,杨进辉,等.胶东中生代构造体制转折过程中流体演化和金的大规模成矿[J].岩石学报,2005,21(5):1317-1328.
Fan Hongrui , Hu Fangfang , Yang Jinhui ,et al.Fluid evolution and large-scale gold metallogeny during Mesozoic tectonic transition in the eastern Shandong Province[J].Acta Petrologica Sinica,2005,21(5):1317-1328.
58 徐永昌,沈平,刘文汇,等.天然气中稀有气体地球化学[M].北京:科学出版社,1998.
Xu Yongchang , Shen Ping , Liu Wenhui ,et al.Geochemistry for Rare Gas in the Natural Gases[M].Beijing:Science Press,1998.
59 Song M C , Li S Z , Santosh M ,et al.Types,characteristics and metallogenesis of gold deposits in the Jiaodong Peninsula,Eastern North China Craton[J].Ore Geology Reviews,2015,65:612-625.
60 Yang L Q , Deng J , Goldfarb R J ,et al.40Ar-39Ar geochronological constraints on the formation of the Dayingezhuang gold deposit:New implications for timing and duration of hydrothermal activity in the Jiaodong gold province,China[J].Gondwana Research,2014,25(4):1469-1483.
61 丁正江,孙丰月,刘福来,等.胶东中生代动力学演化及主要金属矿床成矿系列[J].岩石学报,2015,31(10):3045-3080.
Ding zhengjiang , Sun Fengyue , Liu Fulai ,et al.Mesozoic geodynamic evolution and metallogenic series of major metal deposits in Jiaodong Peninsula,China[J].Acta Petrologica Sinica,2015,31(10):3045-3080.
62 宋英昕,宋明春,孙伟清,等.胶东金矿成矿时代及区域地壳演化——基性脉岩的SHRIMP锆石U-Pb年龄及其地质意义[J].地质通报,2018,37(5):908-919.
Song Yingxin , Song Mingchun , Sun Weiqing ,et al.Metallogenic epoch and regional crust evolution in the Jiaodong gold deposit,Shandong Province:Evidence from SHRIMP zircon U-Pb ages of mafic dykes[J].Geological Bulletin of China,2018,37(5):908-919.
63 Bi S J , Zhao X F .40Ar/39Ar dating of the Jiehe gold deposit in the Jiaodong Peninsula,eastern North China Craton:Implications for regional gold metallogeny[J].Ore Geology Reviews,2017,86:639-651.
64 Hu F F , Fan H R , Yang J H ,et al.Mineralizing age of the Rushan lode gold deposit in the Jiaodong Peninsula:SHRIMP U–Pb dating on hydrothermal zircon[J].Chinese Science Bulletin,2004,49(15):1629-1636.
65 李厚民,毛景文,沈远超,等.胶西北东季金矿床钾长石和石英的Ar-Ar年龄及其意义[J].矿床地质,2003,22(1):72-77.
Li Houmin , Mao Jingwen , Shen Yuanchao ,et al.Ar-Ar ages of K-feldspar and quartz from Dongji gold deposit,northwest Jiaodong,and their significance[J].Mineral Deposits,2003,22(1):72-77.
66 杨进辉,周新华,陈立辉.胶东地区破碎带蚀变岩型金矿时代的测定及其地质意义[J].岩石学报,2000,16(3):454-458.
Yang Jinhui , Zhou Xinhua , Chen Lihui .Dating of gold mineralization for super-large altered tectonite-type gold deposits in northwestern Jiaodong Peninsula and its implications for gold metellogeny[J].Acta Petrologica Sinica,2000,16(3):454-458.
67 Yang J H , Zhou X H .The Rb-Sr isochron of ore and pyrite sub-samples from Linglong gold deposit,Jiaodong Peninsula,eastern China and their geological significance[J].Chinese Science Bulletin,2000,45(24):2272-2276.
68 Yang J H , Zhou X H .Rb-Sr,Sm-Nd and Pb isotope systematics of pyrite:implications for the age and genesis of lode gold deposits[J].Geology,2001,29(8):711-714.
69 Zhang L C , Shen Y C , Liu T B ,et al.40Ar/39Ar and Rb-Sr isochron dating of the gold deposits on northern margin of the Jiaolai Basin,Shandong,China[J].Science China:Earth Science,2003,46(7):708-718.
70 Zhang X O , Cawood P A , Wilde S A ,et al.Geology and timing of mineralization at the Cangshang gold deposit,north-western Jiaodong Peninsula,China[J].Mineralium Deposit,2003,38(2):141-153.
[1] 潘彤,王德福. 初论青海省金矿成矿系列[J]. 黄金科学技术, 2018, 26(4): 423-430.
[2] 张宝林,苗雅娜,苏艳平,李会中. “地物化三场异常耦合理论”及其在隐伏金多金属矿床定位预测中的应用[J]. 黄金科学技术, 2018, 26(4): 431-442.
[3] 王国光,赵超,倪培,刘政. 钦杭成矿带金山造山型金矿成矿年代学研究[J]. 黄金科学技术, 2018, 26(4): 443-453.
[4] 张蕾蕾,张静,王琦崧,陈良,陈叙安. 熊耳山地区槐树坪金矿床黄铁矿特征及其地质意义[J]. 黄金科学技术, 2018, 26(4): 481-491.
[5] 肖风利, 曾庆栋, 马凤山, 王昭坤, 孙之夫, 孙宗峰. 胶东西北部重要金成矿断裂带特征[J]. 黄金科学技术, 2018, 26(4): 396-405.
[6] 杜胜江, 温汉捷, 秦朝建, 卢树藩, 燕永锋, 杨光树. 滇东南老君山矿集区三保锰银矿床碳氧同位素特征及其意义[J]. 黄金科学技术, 2018, 26(3): 261-269.
[7] 张琪彬, 张朋, 徐忠华, 刘向东, 张亮亮, 王斌, 王珊珊. 山东牟平阎家疃金矿床地质特征及成因探讨[J]. 黄金科学技术, 2018, 26(3): 279-288.
[8] 陈懋弘, 谢贤洋, 马克忠. 贵州泥堡卡林型金矿断控型矿体的地层和岩性条件研究[J]. 黄金科学技术, 2018, 26(2): 131-142.
[9] 曲晖, 王佰义, 王建民, 李成禄, 徐国战, 王卓. 土壤地球化学测量在永新金矿勘查中的应用及找矿效果研究[J]. 黄金科学技术, 2018, 26(2): 143-152.
[10] 张健,杨兴科*,晁会霞,何虎军,韩珂,杨龙伟,李斌. 南秦岭石泉—汉阴北部金矿带矿化蚀变特征[J]. 黄金科学技术, 2017, 25(6): 21-30.
[11] 郑慕婷,张术根,贺忠春. 湖南康家湾金银多金属矿床金银赋存状态及其与成矿演化的关系[J]. 黄金科学技术, 2017, 25(6): 31-42.
[12] 梁永科,王德恭,赵杰. 湖南玉横塘金矿区地质特征及找矿前景分析[J]. 黄金科学技术, 2017, 25(6): 43-51.
[13] 高帅,曾庆栋,于昌明,邢宝山,荆林海,叶杰,范宏瑞,杨奎锋. 遥感及综合物探方法用于山东招远南部隐伏成矿侵入体的空间定位[J]. 黄金科学技术, 2017, 25(5): 1-10.
[14] 韩珂,杨兴科*,张健,胡国朝. 陕南汉阴黄龙金矿脆—韧性剪切带特征及其对成矿的控制作用[J]. 黄金科学技术, 2017, 25(5): 18-29.
[15] 王晓青,杨兴科,芮会超. 内蒙古岱王山金矿黄铁矿形态标型及其变化规律与找矿意义[J]. 黄金科学技术, 2017, 25(5): 39-46.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 王晖. 提高罗盘仪导线测量精度的探讨[J]. J4, 2009, 17(4): 47 -49 .
[2] 曾妙先. 金矿石品位和磨矿细度、浮选指标的关系研究[J]. J4, 2003, 11(4): 28 -34 .
[3] 陈晓吾. 浅析GPS 高程测量[J]. J4, 2011, 19(1): 77 -79 .
[4] 刘新会,杨登美,王伟峰,郑卫军. 南秦岭金龙山金矿构造控矿作用及成矿模式研究[J]. 黄金科学技术, 2013, 21(6): 1 -10 .
[5] 王立新,贾磊,吴杰,刘冲昊,杨隆勃. 陕西铧厂沟金矿床地质特征及成矿规律[J]. 黄金科学技术, 2013, 21(6): 11 -21 .
[6] 郭红乐,董俊超,刘江领,刘新会,李福生,马永兵. 甘肃礼岷成矿带西段金成矿条件及成矿预测[J]. 黄金科学技术, 2013, 21(6): 22 -29 .
[7] 王斌,张栋,范俊杰,张峰,潘爱军,朱鹏. 混合稀释剂法测定岩石样品中Sr-Nd同位素组成——以新疆松喀尔苏铜(金)矿区含矿花岗斑岩为例[J]. 黄金科学技术, 2014, 22(2): 24 -30 .
[8] 雷慈坤,唐谷清,赵海燕,黄锦锦,孙春霞. 内蒙古翁牛特旗张家沟银矿床地质特征及银赋存状态研究[J]. 黄金科学技术, 2014, 22(4): 14 -19 .
[9] 王虎,刘洋,秦香伟,亓传铎. 中矿再磨及流程改造提高金精矿品位的实践[J]. 黄金科学技术, 2014, 22(6): 55 -59 .
[10] 田润青,刘云华,田民民,魏居珍,滕飞,李欢,李兴. 陕西某微细粒浸染型金矿选矿试验研究[J]. 黄金科学技术, 2016, 24(6): 102 -106 .