img

QQ群聊

img

官方微信

高级检索

黄金科学技术 ›› 2020, Vol. 28 ›› Issue (4): 465-478.doi: 10.11872/j.issn.1005-2518.2020.04.083

• 矿产勘查与资源评价 •    下一篇

非洲大陆金矿分布特征与勘查建议

江思宏1(),张莉莉1,刘翼飞1,李高峰1,季根源1,2   

  1. 1.中国地质科学院矿产资源研究所,自然资源部成矿作用与资源评价重点实验室,北京 100037
    2.自然资源实物地质资料中心,河北 廊坊 065201
  • 收稿日期:2020-04-30 修回日期:2020-05-20 出版日期:2020-08-31 发布日期:2020-08-27
  • 作者简介:江思宏(1968-),男,安徽肥西人,研究员,博士生导师,从事金属矿床成矿规律研究工作。jiangsihong1@163.com
  • 基金资助:
    中国地质调查局项目“境外大型矿产资源基地及资源潜力评价”(DD20190437)

Distribution Characteristics of Gold Deposits in Africa and Exploration Suggestions

Sihong JIANG1(),Lili ZHANG1,Yifei LIU1,Gaofeng LI1,Genyuan JI1,2   

  1. 1.MNR Key Laboratory of Metallogeney and Mineral Assessment,Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China
    2.Cores and Samples Center of Natural Resources,Langfang 065201,Hebei,China
  • Received:2020-04-30 Revised:2020-05-20 Online:2020-08-31 Published:2020-08-27

摘要:

非洲是全球最为重要的金矿产区,也是吸引金矿勘查投资的热点地区之一。文章对非洲大陆金矿床的时空分布特点进行了简要总结。非洲大陆的矿床类型众多,包括砾岩型、造山型、VMS型、侵入岩型、斑岩型、浅成低温热液型和IOCG型等,且以前2种类型为主。金矿床主要分布在古老的克拉通,尤其是非洲南部的卡拉哈里克拉通和西北部的西非克拉通,这2个地区都是世界著名的金矿产区。少部分金矿产出于新元古代造山带上,如努比亚地盾,在其他泛非期的造山带上也有金矿床零星产出。非洲大陆上金矿的形成时代主要集中在3个时期,即太古宙、古元古代和新元古代。南非兰德盆地砾岩型金矿形成规模大,可能主要与其古沉积环境有关,即处于冲积的辫状河平原;而西非克拉通作为全球最重要的古元古代金矿产区,金的富集可能主要与地层中含有大量的碳质有关。尽管在非洲大陆已经发现了很多世界级的金矿床,但是其找矿潜力仍然很大,尤其是造山型金矿床,因为无论是非洲古老的克拉通还是克拉通周边产出的新元古代造山带都是造山型金矿床形成的有利构造环境。对于在非洲大陆开展金矿找矿勘查,建议在加强已有金矿床深部找矿的基础上,进一步关注半隐伏—隐伏矿床的寻找,尤其是在西非克拉通和刚果克拉通上的浅覆盖区,利用先进的物化遥手段,有望取得金矿找矿的突破。

关键词: 金矿床, 造山型, 砾岩型, 分布特征, 勘查建议, 非洲

Abstract:

Africa is the most important gold producing area in the world,and one of the hot spots to attract gold exploration investment as well.Based on the systematic collection and processing of the advances of the previous research on typical gold deposits and regional metallogenesis in the African continent,the spatial and temporal distribution of gold deposits in the African continent is summarized briefly in this article,which made the achievements below.The African continent consists mainly of four ancient cratons (i.e.Kalahari Craton,West Africa Craton,Congo Craton,and Sahara Meta-Craton) and Neoproterozoic orogenic belts developed around these cratons,as well as some Mesozoic basins developed on the cratons.The gold deposits predominantly occur in the ancient craton,especially in the Kalahari Craton in southern Africa and West African Craton in north-western Africa,where are the world famous gold producing areas.A small proportion of gold deposits are distributed in the Neoproterozoic orogenic belts,such as the Nubian Shield,and other Pan-African orogenic belts.There are many types of gold deposits in African,including conglomerate,orogenic,VMS,intrusion-related,porphyry,epithermal and IOCG types,with the former two being the most important types.The ore-forming age of gold deposits in Africa is mainly concentrated in three periods,i.e.Archean,Paleoproterozoic and Neoproterozoic.The enrichment of huge-sized conglomerate-type gold deposits in the Witwatersrand Basin of South Africa may be mainly related to their paleo-sedimentary environment,i.e.the alluvial braided river plain,while the gold enrichment in West African Craton,as the most important Paleoproterozoic gold region in the world,mainly attributes to the large amount of carbonaceous in the strata.Although many world-class gold deposits have been found in the African continent,their prospecting potential remains significant,especially in the search for orogenic gold deposits,as both the ancient craton and the Neoproterozoic orogenic belt occurring around the craton are favorable tectonic environments for the formation of orogenic gold deposits.For the gold exploration in the African continent,it is suggested that not only pay much attention to the deep prospecting of discovered gold deposits,but also to searching for the semi-buried and buried deposits,especially in the shallow covered areas of West African Craton and Congo Craton.By means of advanced geophysical,geochemical and remote sensing,the breakthrough of gold prospecting is expected.

Key words: gold deposit, orogenic type, conglomerate type, distribution characteristics, exploration suggestion, Africa

中图分类号: 

  • P618.51

图1

非洲大陆的主要构造单元[36]DM-Damara造山带;GP-Gariep造山带;LF-卢菲里安褶皱带;MA-Mauretanides造山带;NS-努比亚地盾;MB-Mozambique造山带;RB-Rokelides造山带;SD-Saldania造山带;WC-West Congo造山带;ZB-Zambezi造山带"

图2

兰德盆地地质简图和金矿田分布图[11]1.金矿田(①-Evander;②-East Rand;③-Central Rand;④-West Rand;⑤-South Deep;⑥-Western Areas;⑦-Carletonville;⑧-Klerksdorp;⑨-Welkom);2.断层;3.Central Rand群(属兰德超群);4.West Rand群(属兰德超群);5.Dominion群;6.太古宙花岗岩;7.太古宙绿岩"

图3

西非克拉通主要金矿床分布简图(据文献[21,53]修改)①-Eglab构造单元;②-Yetti构造单元;③-Daomeyan构造单元;④-Baoulé-Mossi构造单元;⑤-Kenema-Man构造单元;⑥-Kédougou-Kénébia Inlier构造单元;⑦-Rokelides构造单元;⑧-Bassarides构造单元;⑨-Mauritanides构造单元;1.晚于古元古代岩石;2.泛非/华力西期构造带;3.古元古代岩石;4.太古宙岩石;5.西非克拉通推测界线;6.金矿床"

表1

西非克拉通金资源量大于100 t的主要金矿床[21]"

矿床名称国家矿石量 /(×106 t)金品位 /(×10-6金资源量 /t
Tongon科特迪瓦45.402.64120.0
Ahafo加纳270.71.68454.0
Iduapreim加纳150.211.41211.6
Obuasi加纳197.345.791 143.2
Damang加纳129.62.02261.8
Tarkwa加纳345.21.31452.2
Bogoso/Prestea加纳64.83.09200.2
Wassa/HBB加纳67.61.60108.5
EGM加纳208.211.1229.2
Esaase加纳91.151.73158.0
Obotan加纳66.692.1140.5
Akyem加纳143.21.65236.4
Siguiri几内亚264.950.73194.1
Sadiola马里414.021.69700.7
Loulo马里72.964.23308.4
Gounkoto马里30.814.66143.5
Syama马里49.4252.7134.6
Massawa塞内加尔40.692.75112.1
Essakane布基纳法索180.9410.89160.3
Kiaka布基纳法索189.020.99186.9
Bomboré布基纳法索158.21.03163.6
Karma布基纳法索111.11.04115.8
Inata布基纳法索106.41.37146.3
Bissa布基纳法索140.6761.12157.6
Mana布基纳法索91.9272.28209.8
Batie West-Konkera布基纳法索59.21.76104.1
Banfora Group布基纳法索105.61.3142.3
Wona-Kona布基纳法索49.962.27113.4

图4

阿拉伯—努比亚地盾金矿床(点)分布图(据文献[2]修改)1.金矿床(点)(包括造山型绘图VMS型金矿);2.正在开采的金矿山;3.湖泊;4.古生界—新生界;5.阿拉伯—努比亚地盾新元古代年轻地壳;6.莫桑比克带;7.新元古代之前的岩石;8阿拉伯—努比亚地盾界线"

图5

坦桑尼亚克拉通金矿床分布图(据文献[15,22]修改)超级地体(由北向南):ELVST-East Lake Victoria;MLEST-Mwanza-Lake Eyasi;LNST-Lake Nyanza;MMST-Moyowosi-Manyoni;绿岩带:SU-Sukumaland绿岩带;NZ-Nzega绿岩带;SM-Shynianga-Malita绿岩带;IS-Iramba-Sekenke绿岩带;KF-Kilimafedha绿岩带;MM-Musoma-Mara绿岩带;1.现代火山岩;2.新近纪火山岩;3.元古宙活动带;4.太古宙花岗岩和片麻岩;5.太古宙绿岩带;6.超级地体界线;7.金矿床(年产金约0.5×106盎司);8.金矿点"

1 Zoheir B,Emam A,Pitcairn I K,et al.Trace elements and isotope data of the Um Garayat gold deposit,Wadi Allaqi district,Egypt[J].Mineralium Deposita,2019,54:101-116.
2 Zoheir B A,Johnson P R,Goldfarb R J,et al.Orogenic gold in the Egyptian Eastern Desert:Widespread gold mineralization in the late stages of Neoproterozoic orogeny[J].Gondwana Research,2019,75:184-217.
3 Helmy H M,Kaindl R,Fritz H,et al.The Sukari gold mine,Eastern Desert—Egypt:Structural setting,mineralogy and fluid inclusion study[J].Mineralium Deposita,2004,39(4):495-511.
4 Goldfarb R J,Groves D I,Gardoll S.Orogenic gold and geologic time:A global synthesis[J].Ore Geology Reviews,2001,18(1/2):1-75.
5 Kirk J,Ruiz J,Chesley J,et al.A detrital model for the origin of gold and sulfides in the Witwatersrand basin based on Re-Os isotopes[J].Geochimica et Cosmochimica Acta,2001,65(13):2149-2159.
6 Meier D L,Heinrich C A,Watts M A.Mafic dikes displacing Witwatersrand gold reefs:Evidence against metamorphic-hydrothermal ore formation[J].Geology,2009,37(7):607-610.
7 Schaefer B F,Pearson D G,Rogers N W,et al.Re-Os isotope and PGE constraints on the timing and origin of gold mineralisation in the Witwatersrand Basin[J].Chemical Geology,2010,276(1/2):88-94.
8 Depiné M,Frimmel H E,Emsbo P,et al.Trace element distribution in uraninite from Mesoarchaean Witwatersrand conglomerates (South Africa) supports placer model and magmatogenic source[J].Mineralium Deposita,2013,48(4):423-435.
9 Phillips G N,Powell R.Hydrothermal alteration in the Witwatersrand goldfields[J].Ore Geology Reviews,2015,65:245-273.
10 Mathur R,Gauert C,Ruiz J,et al.Evidence for mixing of Re-Os isotopes at < 2.7 Ga and support of a remobilized placer model in Witwatersrand sulfides and native Au[J].Lithos,2013,164-167:65-73.
11 Frimmel H E.The Witwatersrand Basin and Its Gold Deposits[M]//Kröner A,Hofmann A.The Archaean Geology of the Kaapvaal Craton,Southern Africa.Berlin:Springer,2019.
12 da Costa G,Hofmann A,Agangi A.A revised classification scheme of pyrite in the Witwatersrand Basin and application to placer gold deposits[J].Earth-Science Reviews,2020,201:103064.
13 Agangi A,Hofmann A,Rollion-Bard C,et al.Gold accumulation in the Archaean Witwatersrand Basin,South Africa—Evidence from concentrically laminated pyrite[J].Earth-Science Reviews,2015,140:27-53.
14 Klemm D D,Kräutner H G.Hydrothermal alteration and associated mineralization in the Freda-Rebecca gold deposit ± Bindura District,Zimbabwe[J].Mineralium Deposita,2000,35:90-108.
15 Kabete J M,Groves D I,McNaughton N J,et al.A new tectonic and temporal framework for the Tanzanian Shield:Implications for gold metallogeny and undiscovered endowment[J].Ore Geology Reviews,2012,48:88-124.
16 Chinnasamy S S,Uken R,Reinhardt J,et al.Pressure,temperature,and timing of mineralization of the sedimentary rock-hosted orogenic gold deposit at Klipwal,southeastern Kaapvaal Craton,South Africa[J].Miner Deposita,2015,50:739-766.
17 Hein K A A,Matsheka I R,Bruguier O,et al.The Yatela gold deposit:2 billion years in the making[J].Journal of African Earth Sciences,2015,112:548-569.
18 Salvi S,Sangaré A,Driouch Y,et al.The Kalana vein-hosted gold deposit,southern Mali[J].Ore Geology Reviews,2016,78:599-605.
19 Augustin J,Gaboury D,Crevier M.Structural and gold mineralizing evolution of the world-class orogenic Mana district,Burkina Faso:Multiple mineralizing events over 150 million years[J].Ore Geology Reviews,2017,91:981-1012.
20 Fougerouse D,Micklethwaite S,Ulrich S,et al.Evidence for two stages of mineralization in west Africa’s largest gold deposit:Obuasi,Ghana[J].Economic Geology,2017,112(1):3-22.
21 Goldfarb R J,André-Mayer A S,Jowitt S M,et al.West Africa:The World’s premier Paleoproterozoic gold province[J].Economic Geology,2017,112(1):123-143.
22 Sanislav I V,Brayshaw M,Kolling S L,et al.The structural history and mineralization controls of the world-class Geita Hill gold deposit,Geita Greenstone Belt,Tanzania[J].Mineralium Deposita,2017,52:257-279.
23 Smit C A,Van Reenen D D,Mccourt S,et al.Hypozonal orogenic gold mineralization in the Giyani Goldfield,Northern Kaapvaal Craton/ Limpopo Complex[J].South African Journal of Geology,2019,122(4):455-488.
24 Yao Y,Murphy P J,Robb L J.Fluid characteristics of granitoid-hosted gold deposits in the Birimian Terrane of Ghana:A fluid inclusion microthermometric and Raman spectroscopic study[J].Economic Geology,2001,96(7):1611-1643.
25 Allibone A,Teasdale J,Cameron G,et al.Timing and structural controls on gold mineralization at the Bogoso gold mine,Ghana,West Africa[J].Economic Geology,2002,97(5):949-969.
26 Coulibaly Y,Boiron M C,Cathelineau M,et al.Fluid immiscibility and gold deposition in the Birimian quartz veins of the Angovia deposit(Yaouré,Ivory Coast)[J].Journal of African Earth Sciences,2008,50(2/3/4):234-254.
27 Dziggel A,Wulff K,Kolb J,et al.Processes of high-T fluid-rock interaction during gold mineralization in carbonate-bearing metasediments:The Navachab gold deposit,Namibia[J].Mineralium Deposita,2009,44:665-687.
28 Amponsah P O,Salvi S,Béziat D,et al.Geology and geochemistry of the shear-hosted Julie gold deposit,NW Ghana[J].Journal of African Earth Sciences,2015,112:505-523.
29 Kříbek B,Sýkorová I,Machovič V,et al.The origin and hydrothermal mobilization of carbonaceous matterasso-ciated with Paleoproterozoic orogenic-type gold deposits of West Africa[J].Precambrian Research,2015,270:300-317.
30 Perrouty S,Jessell M W,Bourassa Y,et al.The Wassa deposit:A poly-deformed orogenic gold system in southwest Ghana—Implications for regional exploration[J].Journal of African Earth Sciences,2015,112:536-547.
31 Büttner S H,Reid W,Glodny J,et al.Fluid sources in the Twangiza-Namoya gold belt (Democratic Republic of Congo):Evidence from tourmaline and fluid compositions,and from boron and Rb-Sr isotope systematics[J].Precambrian Research,2016,280:161-178.
32 Lambert-Smith J S,Lawrence D M,Vargas C A,et al.The Gounkoto Au deposit,West Africa:Constraints on ore genesis and volatile sources from petrological,fluid inclusion and stable isotope data[J].Ore Geology Reviews,2016,78:606-622.
33 Adomako-Ansah K,Mizuta T,Ishiyama D,et al.Nature of ore-forming fluid and formation conditions of BIF-hosted gold mineralization in the Archean Amalia Greenstone Belt,South Africa:Constraints from fluid inclusion and stable isotope studies[J].Ore Geology Reviews,2017,89:609-626.
34 Argapadmi W,Toth E R,Fehr M A,et al.Silver Isotopes as a Source and Transport Tracer for Gold:A Reconnaissance Study at the Sheba and New Consort Gold Mines in the Barberton Greenstone Belt,Kaapvaal Craton,South Africa[J].Economic Geology,2018,113(7):1553-1570.
35 Béziat D,Dubois M,Debat P,et al.Gold metallogeny in the Birimian craton of Burkina Faso (West Africa) [J].Journal of African Earth Sciences,2008,50(2/3/4):215-233.
36 Fagbohuna B J,Omitogun A A,Bamisaiye O A,et al.Gold potential of the Pan African Trans-Sahara belt and prospect for further Exploration[J].Ore Geology Reviews,2020,116:103260.
37 李俊生,樊克锋,马春阳.非洲塞拉利昂共和国北部Makong地区砂金矿特征及找矿方向探讨[J].长春工程学院学报(自然科学版),2010,11(2):66-68.
Li Junsheng,Fan Kefeng,Ma Chunyang.Discussion on the characteristic and prospecting direction of gold depo-sit in Makong—The North of Sierra Leone republic of Africa[J].Journal of Changchun Institute of Technology (Natural Science Edition),2010,11(2):66-68.
38 任军平,许康康,相振群,等.南非维特沃特斯兰德盆地绍斯迪普金矿床地质特征、成矿模式和找矿模型[J].地质通报,2015,34(6):1217-1226.
Ren Junping,Xu Kangkang,Xiang Zhenqun,et al.Geological characteristics,metallogenic model and prospecting criteria of the South Deep gold deposit in Witwatersrand Basin,South Africa[J].Geological Bulletin of China,2015,34(6):1217-1226.
39 江伟华,卿芸,胡晓丽,等.津巴布韦卢比(Ruby)矿床—南部非洲一典型的BIF型金矿床[J].矿产勘查,2017,8(1):161-164.
Jiang Weihua,Qing Yun,Hu Xiaoli,et al.Ruby gold deposit of Zimbabwe:A typical BIF-hosted gold deposit in southern Africa[J].Mineral Exploration,2017,8(1):161-164.
40 张毅,岳鹏军,谭康雨,等.南非某金矿矿床地质特征及找矿前景[J].世界有色金属,2019(24):83-85.
Zhang Yi,Yue Pengjun,Tan Kangyu,et al.Geological characteristics and prospecting prospects of a gold deposit in South Africa[J].World Nonferrous Metal,2019(24):83-85.
41 王杰,任军平,何胜飞,等.南非主要金矿集区研究现状及存在问题[J].地质论评,2014,60(5):997-1008.
Wang Jie,Ren Junping,He Shengfei,et al.Review of studies on the gold deposit-accumulated area in South Africa[J].Geological Review,2014,60(5):997-1008.
42 魏浩,徐九华,王建雄,等.非洲东北部阿拉伯-努比亚地盾(ANS)构造演化与金成矿作用[J].地质与勘探,2015,51(2):383-394.
Wei Hao,Xu Jiuhua,Wang Jianxiong,et al.Tectonic evolution and gold mineralization in the Arabian Nubian Shield(ANS),Northeastern Africa[J].Geology and Exploration,2015,51(2):383-394.
43 孙宏伟,唐文龙,刘晓阳,等.非洲东南部造山型金矿成矿环境与资源潜力分析[J].吉林大学学报(地球科学版),2018,48(6):1654-1668.
Sun Hongwei,Tang Wenlong,Liu Xiaoyang,et al.Metallogenic environment and resource potential of orogenic gold deposit in Southeast Africa[J].Journal of Jilin University(Earth Science Edition),2018,48(6):1654-1668.
44 姚伟,刘亮明.遥感技术在北非努比亚地盾Wadi Halfa地区金矿勘查中的应用[J].地质与勘探,2014,50(1):167-172.
Yao Wei,Liu Liangming.Application of the remote sensing technique to gold exploration in Wadi Halfa district,Nubia shield of North Africa[J].Geology and Exploration,2014,50(1):167-172.
45 居维伟,贾 磊,刘小胡,等.非洲加纳上东部省ZG区变质热液型金矿地质勘查的技术和方法[J].世界有色金属,2018(14):164-166.
Ju Weiwei,Jia Lei,Liu Xiaohu,et al.Technology and method for geological exploration of metamorphic hydrothermal gold deposits in ZG area,upper Garner,eastern Africa[J].World Nonferrous Metal,2018(14):164-166.
46 Kröner A,Hoffmann J E,Wong J M,et al.Archaean Crystalline Rocks of the Eastern Kaapvaal Craton[M]//Krö-ner A,Hofmann A.The Archaean Geology of the Kaapvaal Craton,Southern Africa.Berlin:Springer,2019.
47 Rollinson H.Archaean crustal evolution in West Africa:A new synthesis of the Archaean geology in Sierra Leone,Liberia,Guinea and Ivory Coast[J].Precambrian Research,2016,281:1-12.
48 Grenholm M.The global tectonic context of the ca.2.27-1.96 Ga Birimian Orogen-Insights from comparative studies,with implications for supercontinent cycles[J].Earth-Science Reviews,2019,193:260-298.
49 Lenoir J L,Liégeois J P,Theunissen K,et al.The Palaeoproterozoic Ubendian shear belt in Tanzania,geochronology and structure[J].Journal of African Earth Sciences,1994,19(3):169-184.
50 Frimmel H E.Earth’s continental crustal gold endowment[J].Earth and Planetary Science Letters,2008,267(1/2):45-55.
51 Robertson M,Peters L.Gold in West Africa;what does the future hold?[C]//35th International Geological Congress,Abstracts.Alexandria:The American Geosciences Institute,2016.
52 Augustin J,Gaboury D,Crevier M.The world-class Wona-Kona gold deposit,Burkina Faso[J].Ore Geology Reviews,2016,78:667-672.
53 Markwitz V,Hein K A A,Miller J.Compilation of West African mineral deposits:Spatial distributionand mineral endowment[J].Precambrian Research,2016,274:61-81.
54 Billay A Y,Kisters A F M,Meyer F M,et al.The geology of the Lega Dembi gold deposit,southern Ethiopia:Implications for Pan-African gold exploration[J].Mineralium Deposita,1997,32:491-504.
55 Bierlein F P,Potma W,Cernuschi F,et al.New insights into the evolution and age of the Neoproterozoic Jebel Ohier Porphyry Copper Deposit,Red Sea Hills,Northeastern Sudan[J].Economic Geology,2020,115(1):1-31.
56 Pirajno F,Jacob R E.Gold mineralisation in the intracontinental branch of the Damara Orogen,Namibia:A preliminary survey[J].Journal of African Earth Sciences,1991,13(3/4):305-311.
57 Buchholz P,Herzig P,Friedrich G,et al.Granite-hosted gold mineralization in the Midlands greenstone belt:A new type of low-grade gold deposit in Zimbabwe[J].Mineralium Deposita,1998,33:437-460.
58 章振根.南非维特瓦特斯兰德金矿床[J].黄金科学技术,1990(2):29-31.
Zhang Zhengen.The Witwatersand gold deposits in South Africa[J].Gold Science and Technology,1990(2):29-31.
59 Ballo I,Hein K A A,Guindo B,et al.The Syama and Tabakoroni goldfields,Mali[J].Ore Geology Reviews,2016,78:578-585.
60 Salvi S,Amponsah P O,Siebenaller L,et al.Shear-related gold mineralization in Northwest Ghana:The Julie deposit[J].Ore Geology Reviews,2016,78:712-717.
61 Heron K,Jessell M,Benn K,et al.The Tasiast deposit,Mauritania[J].Ore Geology Reviews,2015,78:564-572.
[1] 秦运忠, 宋海军. 广西乐业县岩旦—岩堂金矿床找矿模型及成矿预测[J]. 黄金科学技术, 2020, 28(3): 317-327.
[2] 谢也真,曹平,陈昊然. 滥泥坪铜矿三维地应力测量及巷道布置优化研究[J]. 黄金科学技术, 2019, 27(6): 862-870.
[3] 张克川,罗清威,义爱文,秦德雨,权成,杨继兵. 坦桑尼亚PL7184金矿床矿石特征与金的赋存状态[J]. 黄金科学技术, 2019, 27(6): 826-834.
[4] 郭剑衡, 冷成彪, 张兴春, 张伟, 尹崇军, 张陆佳, 田振东. 滇西北烂泥塘斑岩铜金矿床铁氧化物LA-ICP-MS微量元素特征及其地质意义[J]. 黄金科学技术, 2019, 27(5): 659-677.
[5] 孙伟清,刘燊,冯彩霞,范焱,刘永昌. 招平断裂带中段金矿床控矿条件与成矿规律研究[J]. 黄金科学技术, 2019, 27(3): 315-327.
[6] 惠伟光,雷明选,夏元鹏,张晓斌,孙青,段绪省. 甘肃肃北县460金矿床地质特征及原生晕地球化学找矿预测[J]. 黄金科学技术, 2018, 26(5): 570-585.
[7] 宋明春,宋英昕,丁正江,李世勇. 胶东金矿床:基本特征和主要争议[J]. 黄金科学技术, 2018, 26(4): 406-422.
[8] 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.
[9] 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.
[10] 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.
[11] 宋英昕,宋明春,丁正江,魏绪峰,徐韶辉,李杰,谭现峰,李世勇,张照录, 焦秀美,胡弘,曹佳. 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.
[12] 徐忠华,王福江,周明岭,白宜娜,赵成乐,胡秉谦. 胶东磨山金矿床主要金属矿物的矿物学特征及矿床成因研究[J]. 黄金科学技术, 2017, 25(3): 28-37.
[13] 汪超,谷玉明,胡西顺,门文辉,杨海涛,吴涛,王瑜亮,赵彦峰. 陕西三官庙—韭菜沟地区钠长岩与金矿床地质特征及找矿方向[J]. 黄金科学技术, 2017, 25(1): 35-45.
[14] 汪超,门文辉,吴涛,张骁富,李英,胡西顺. 陕西三官庙金矿床地质特征、原生晕分带特征及其找矿意义[J]. 黄金科学技术, 2016, 24(6): 39-48.
[15] 曹东宏,崔龙,辛小军,朝银银. 西秦岭马坞金矿床韧性剪切带构造控矿特征[J]. 黄金科学技术, 2016, 24(6): 24-31.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 闫杰, 覃泽礼, 谢文兵, 蔡邦永. 青海南戈滩—乌龙滩地区多金属地质特征与找矿潜力[J]. J4, 2010, 18(4): 22 -26 .
[2] 宋贺民, 冯喜利, 丁宪华. 太行山北段交界口矿区地质地球化学特征及找矿方向[J]. J4, 2010, 18(3): 54 -58 .
[3] 李淑芳, 于永安, 朝银银, 王美娟, 张岱, 刘君, 孙亮亮. 在辽东成矿带找寻层控型金矿床靶区[J]. J4, 2010, 18(3): 59 -62 .
[4] 崔廷军, 逯克思, 庄勇, 傅星. 青海省柴达木盆地南缘金成矿带特征及成矿规律浅析[J]. J4, 2010, 18(3): 63 -67 .
[5] 杨明荣, 牟长贤. 原子荧光法测定化探样品中砷和锑的不确定度评定[J]. J4, 2010, 18(3): 68 -71 .
[6] 张渊, 张洪喜. 山东黄埠岭金矿7号脉地质特征及控矿机理研究[J]. J4, 2010, 18(4): 12 -16 .
[7] 李斌, 邹海洋, 杨牧, 杜高峰, 韦继康, 王天国. 马来西亚吉兰丹州Ulu Sokor金矿地质特征及找矿方向[J]. J4, 2010, 18(4): 17 -21 .
[8] 姜琪, 王荣超. 甘肃枣子沟金矿床形成环境及矿床成因[J]. J4, 2010, 18(4): 37 -40 .
[9] 路明福, 扈守全. 厚大破碎矿体回采技术的对比研究[J]. J4, 2010, 18(4): 62 -64 .
[10] 冷寒松, 邓尧增, 胥华龙, 刘涛, 王卓. 有底柱分段崩落采矿法在焦家金矿的研究与应用[J]. J4, 2010, 18(4): 65 -67 .