Gold Science and Technology
img

Wechat

Adv. Search
Online Submission Peer Review Office Work

J4 ›› 2011, Vol. 19 ›› Issue (2): 13-17.

• article • Previous Articles     Next Articles

Analysis of Ore-controlling Mechanism of Gold Mineralization in Hadamengou Gold Deposit,Inner Mongolia

XIA Dong1,3,NIU Shuyin1,XU Guo2,CHEN Chao1,ZHAO Zhiyuan1,PENG Yuxuan4   

  1. 1.Shijiazhuang University of Economics,Shijiazhuang 050031,Hebei,China；
    2.China University of Geosciences,Beijing 100083,China；
    3.Geological Survey of Inner Mongolia,Huhehaote 010020,Inner Mongolia,China；
    4.Xinjiang Institute of Mineral and Experiment,Wulumuqi 050081,Xinjiang,China
  • Received:2010-02-15 Revised:2011-03-19 Online:2011-04-28 Published:2012-05-11

PDF (PC)

1034

Abstract:

Hadamengou gold mine has a large deposit scale by proven,gold deposit is strictly controlled by tectonic, also has its own unique,such as high gold background values of wallrock,piedmont red fragments altered belts, thick crystal biotite granite pegmatite,and multi-stage intrusion of magma,and it become an indispensable factor in the formation of gold.Take mantle branch theory as a guide,throughcomprehensive study of geological features and other factors,we consider that Hadamengou gold mine belongs to fracture-altered rock typedeposit,wulashan rock Group is an important ore source,EW-trending primary and secondary detachment is the main leading-host structures,multi-stage magmatic activity provide heating,hot water and some minerals for deposit,mineralization is close related with biotite graniticpegmatite and brittle deformation of quartz veins.We discuss metallogenic regularity of deposit,and propose ore prospecting.

Key words: Mantle branch structure, Ore-controlling mechanism of mineralization, Primary and secondary detachment belt, Brittle deformation, Hadamengou gold deposit

CLC Number: 

  • P618.51

［1］牛树银，罗殿文，叶东虎，等.幔枝构造及其成矿规律［M］.北京:地质出版社，1996:1- 124.
［2］苗来成，QIU Yumin，关康，等.哈达门沟金矿床地质特征及其形成时代研究［J］.地质找矿论丛，1999，14（4）:76- 82.
［3］彭大明.内蒙中部专金犷类型及找矿方向［J］.矿床与地质，1991，2（5）:90- 95.
［4］李伟，张月忠.内蒙古乌拉山金矿构造成矿作用浅析［J］.黄金，2003，24（3）:20- 22.
［5］牛树银，孙爱群，邵振国，等.地幔热柱多级演化及其成矿作用［M］.北京:地震出版社，2001：41- 175.
［6］ NIU Shuyin,HOU Quanlin,HOU Zengqian,et al.Cascaded Evolution of Mantle Plumes and Metallogensis of Core and Mantle- derived Elements［

J］.Acta Geologica Sinica,2003,77
（4）：510- 536.
［7］刘伟，戴塔根，傅文杰，等.冀西石湖金矿成矿流体特征［J］.中国地质，2007，34（2）:335- 341.
［8］郎殿有.乌拉山金矿带成矿物质来源的初步研究［J］.矿产与地质，2001，7（1）:55- 61.
［9］梁海军,赵春荣.内蒙古哈达门沟金矿床成矿条件及控矿因素［J］.1999，2（5）:42- 46.
［10］燕守勋，朱振海，黄晓霞，等.阴山中—西段横向构造及其控矿意义的遥感—航磁复合分析［J］.遥感学报，2001，6（5）:454- 459.
［11］牛树银，孙爱群，王宝德.地幔热柱与资源环境［M］.北京:地质出版社，2007:1- 183.
［12］牛树银，罗殿文，叶东虎，等.幔枝构造及其成矿规律［M］.北京:地质出版社，1996:1- 124.
［13］杜乐天.地壳流体与地幔流体间的关系［J］.地学前缘,1996，3（3/4）:341- 346.
［14］毛景文，王志良.中国东部大规模成矿时限及其动力学背景的初步探讨［J］.矿物岩石地球化学通报，2000，19（4）:400- 405.
［15］侯增谦，莫宣学，杨志明，等.青藏高原碰撞造山带成矿作用:构造背景、时空分布和主要类型［J］. 中国地质，2006，33（2）:340- 349.
［16］侯增谦，李红阳.试论幔柱构造与成矿系统———以三江特提斯成矿域为例［J］.矿床地质，1998，17（2）:97- 113.
［17］聂凤军，江思宏.地球演化过程中金属矿产的形成［J］.中国地质，2001，28（4）:24- 31.
［18］牛树银，李红阳，孙爱群，等.幔枝构造理论与找矿实践［M］.北京:地震出版社，2002:1- 243.
［19］牛树银，罗殿文，叶东虎，等.幔枝构造及其成矿规律［M］.北京:地质出版社，1996:1- 124.
［20］陈毓川，毛景文，骆耀南，等.四川大水沟碲（金）矿床地质和地球化学［M］.北京:原子能出版社，1996:1- 146.
［21］VanderHilst R D,Widiyantoro S,Engdahl E R.Evidence for Deep Mantle Circulation from Global Tomography［J］.Nature,1997,386:578- 584.
［22］ZHANG Ronghu，HU Shumin，WANG Jun，et al.Investiga tions of Influx of Deep Fluids Carrying Metal to Earth Cruet and its Experiments

Study［J］.Mineral Deposits，2002,21 （supp）:1095- 1098.
［23］Burek P J, Wanke H.Impacts and Glacio- eustacy,Plate- tectonic Episodes,Geomagnetic Reversals:A Concept to Facilitate DeTection of

Impact Events［J］.Phys.Earth planet.Inter,1988,50:189- 199.
［24］Caldeira K,Rampino MR.The Mid- cretaceous Supcrplume, Carbon Dioxide and Global Warming［J］.Geophys. Res,Lett.,1991,18:22- 99.
［25］郎殿有.乌拉山金矿带成矿物质来源的初步研究［J］.矿产与地质，2001，7（1）:55- 61.
［26］朴寿成，杨永强，胡素清.内蒙古乌拉山金矿原生地球化学异常模式与成因研究［J］.长春地质学院学报，1995，25（4）:399- 403.
［27］郭砚田.内蒙古乌拉山“哈德门沟式”金矿床成矿地质特征［J］.贵金属地质，1992,1（2）：191- 195.
［28］聂凤军，江思宏，刘妍，等.再论内蒙古哈达门沟金矿床的成矿时限问题［J］.岩石学报，2005，21（6）:1719-1728.
［29］孟伟，陈小伍，李蒙文.内蒙古哈达门沟金矿成矿时代及成矿阶段研究［J］.黄金地质，2005，8（4）:14-17.
［30］卫万顺，张宇辉，卿敏,等.中国北方碱性岩型金矿床成因模型研究［J］.黄金地质，2001，7（1）:55-61.
［31］郎殿有.内蒙古乌拉山金矿成矿流体来源、性质和演化［J］.黄金地质，1997，2（3）:24-30.
［32］张宇辉.华北地块含金碱性岩浆源区及其物质来源研究［J］.黄金，2002，23（1）:4-9.
［33］李杰美.内蒙乌拉山金矿脉的特征及其构造分析［J］.黄金，1989，5（10）:14- 17.
［34］李强之,朱成伟,吴尚全,等.内蒙古哈达门沟金矿床钾长石化蚀变特征及其成矿意义［J］.现代地质，1999，13（3）:315- 322.
［35］刘庆生，燕守勋，马超飞,等.内蒙哈达门沟金矿区山前钾化带遥感信息提取［J］.遥感技术与应用，1999,14（3）:7- 11.
［36］霍明远.金的结构模型与地质找矿// 涂光炽,霍明远.金的经济地质学［C］.北京:科学出版社,1991:1- 7.
［37］钟长汀，席忠，赵维宽，等.内蒙古大青山地区金矿床类型、控矿规律及找矿方向［J］.地质调查与研究，2005，28（4）:240- 249.
[1] WANG Yingtian，WANG Shanzhang，LI Bo，HAN Yu. The Metallogenic Regularity and Deep Prospecting of No.1 Vein in Dazhuangzi Gold Deposit，Shandong Province [J]. J4, 2012, 20(4): 123-127.
[2] WANG Xingcun，NIU Shuyin，YAN Jianshe，SUN Weizhi，SUN Aiqun，FENG Jianzhi，CH. Analysis on the Mineralization Structure  of Gold Orefield in Xiaoqinling Midle-orebelt [J]. J4, 2012, 20(4): 96-103.
[3] LI Junfeng，WU Jichun，LIU Weimin，JIANG Shanbo，PENG Hongying，ZHU Suizhou，SHE. Sduty on Metallogenic Regularity and Prospecting of No. 51 Vein in Linglong Gold Mine Field，Shandong Province [J]. J4, 2012, 20(4): 113-116.
[4] KONG Lingzhi，ZHU Suizhou，HAN Yunsong，ZHANG Long，CHU Zhaobo，LI Xinnian，WU. Analysis and Comprehensive of Geophysical Characteristics and Prospecting Prediction in Linglong Fault Belt，Shandong Province [J]. J4, 2012, 20(4): 117-122.
[5] LIU Xinhui，CHEN Caihua，ZHAO Tianxin，ZHANG Keli，CHEN Lizi，LIU Shuang. Primary Geochemistry Characteristics and Metallogenic Prediction of Zhaishang Gold Deposit，West Qinling [J]. J4, 2012, 20(4): 7-15.
[6] LIU Jinyou，LIU Shuliang，GAO Chixing，DUN Meixia. Study on Geochemical Characteristics of Xilaokou Gold Deposit in Shandong Province [J]. J4, 2012, 20(4): 16-20.
[7] JIANG Weiming，QI Fei，MENG Wei，XU Jianbo，LIU Qiujie，LV Jun’en，YUAN Shaobo，SUN Jia. Study on the Metallogenic Regularity and Prospective Prognosis in Linglong-Dongfeng Mining Area，Shandong Province [J]. J4, 2012, 20(4): 21-25.
[8] JIN Nianxian，WANG Junting，SUN Zhifu，LI Wen，LIAO Changxi，SUO Jiancheng，LIU Xiangp. Jiaojia-style Gold Deposit and its Prospecting Direction Controlled by Ductile Shear Zone [J]. J4, 2012, 20(4): 26-32.
[9] HUANG Guanghuan. The Geological Feature and Prospecting Potential Analysis of the Important Metallogenic Belt in Central and Eastern of Inner Mongolia [J]. J4, 2012, 20(4): 33-38.
[10] SUN Jie，LI Ruijun，ZHAO Zhouwei，XU Fen. The Geological Characteristics and Deep Resources Investigation Evaluation of Gold Orebodies in Xiejiagou Mining Area [J]. J4, 2012, 20(4): 39-42.
[11] ZHENG Weijun，LIU Xinhui，CHEN Caihua. 1∶50 000 Stream Sediment Survey Integrative Appraisa in Zhaishang Gold Deposit，Gansu Province [J]. J4, 2012, 20(4): 43-48.
[12] MA Fengshan，ZHAO Haijun，GUO Jie，WANG Jie，WEI Aihua. Numerical Simulation of Pitshaft Stability Induced by Shallow Second Mining in Wang’ershan Mining Area，Shandong Province [J]. J4, 2012, 20(4): 49-53.
[13] WANG Yichun，LI Bo，ZHANG Yonglin，HAN Yu，REN Xiaoming，WANG Zhaomin，WANG Jingcong，Z. Application of Electro-sorption Geochemical Exploration in Deep Orebody Prediction in Mawan Gold Mining Areas [J]. J4, 2012, 20(4): 62-66.
[14] LIU Guige，LI Yanqiu，CHANG Chunjiao，CONG Runxiang，ZHANG Huiyu，CHEN Yonggan，. Research on Comprehensive Anomaly Method of Regional Geochemical Exploration Data Processing [J]. J4, 2012, 20(4): 67-70.
[15] WANG Enjing，GUO Guangjun，ZHAO Rongxin，WANG Yanwei，YU Xiaojie，LV Guangyao，WANG W. Research and Application of the Mineralization Network Structure in Sizhuang Gold Deposit，Shandong Province [J]. J4, 2012, 20(4): 76-80.
Viewed
Full text


Abstract

Cited
  Shared   
  Discussed   
No Suggested Reading articles found!

©2018 Gold Science and Technology　

Telephone：0931-8277791　

E-mail: hjkx@lzb.ac.cn Postcode：730000　

Powered by Beijing Magtech Co. Ltd

陇ICP备17001318号-1