班公湖-怒江成矿带中西段造山型金矿床的成矿地质条件和找矿远景
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  • 英文篇名:Metallogenic conditions and prospecting potential of orogenic gold deposits in the central western part of Bangong Lake-Nujiang metallogenic zone
  • 作者:马国桃 ; 刘洪 ; 黄瀚霄 ; 陈敏华 ; 兰双双 ; 吕梦鸿 ; 解惠
  • 英文作者:MA Guo-tao;LIU Hong;HUANG Han-xiao;CHEN Min-hua;LAN Shuang-shuang;LU Meng-hong;XIE Hui;Chengdu Center,China Geological Survey;Sichuan Institute of Metallurgical Geology and Exploration;
  • 关键词:造山型金矿床 ; 成矿地质条件 ; 找矿远景 ; 班公湖-怒江成矿带
  • 英文关键词:orogenic-type gold deposit;;metallogenic geological condition;;exploration prospect;;Bangong-Nujiang metallogenic zone
  • 中文刊名:TTSD
  • 英文刊名:Sedimentary Geology and Tethyan Geology
  • 机构:中国地质调查局成都地质调查中心;四川省冶金地质勘查院;
  • 出版日期:2017-09-15
  • 出版单位:沉积与特提斯地质
  • 年:2017
  • 期:v.37
  • 基金:基础性公益性地质矿产调查(DD20179604);; 中国地质调查项目(DD20160015、DD20160026);; 国家重点研发计划(2016YFC0600308)联合资助
  • 语种:中文;
  • 页:TTSD201703011
  • 页数:7
  • CN:03
  • ISSN:51-1593/P
  • 分类号:91-97
摘要
本文在阐述班公湖-怒江成矿带中西段成矿地质背景的基础上,重点论述了达查、商旭等造山型金矿床成矿地质条件和控矿因素,综合分析认为木嘎岗日群混杂岩,区域构造转折部位和碰撞初期岩浆岩的复合地带最有利于形成规模较大的造山型金矿床。并以此为依据,划分出尼玛县北-商旭、洞错北-达查、改则县物玛乡北、夏布错北,以及热那错北等5处造山型金矿床成矿远景区。
        In the light of the metallogenic geological conditions and exploration potential,the present paper focuses on geological conditions,ore-controlling factors,isotopic signatures and mineralization age of the Dacha and Shangxu orogenic-type gold deposits in the central-western part of the Bangong-Nujiang metallogenic zone,Xizang.The potential areas favourable for the formation of large-sized orogenic-type gold deposits are restricted to the mélanges of the Muggar Kangri Group,hinge points and magmatic composite zones formed during the early collisional stages. Finally,five exploration prospects are delineated,including northern Nyima-Shangxu,northern Dongco-Dacha, northern Oma in Gerze, northern Xiabuco and northern Renaco in the Bangong-Nujiang metallogenic zone,Xizang.
引文
[1]Groves D I,Goldfarb R J,Gebre-mariam M,et al.Orogenic gold deposits:A proposed classification in the context of their crustal distribution and relationship to other gold deposit types[J].Ore Geology Reviews,1998,13(1):7-27.
    [2]Kerrich R,Goldfarb R,Groves D,et al.The characteristics,origins,and geodynamic settings of supergiant Gold metallogenic provinces[J].Science China Earth Sciences,2000,43(1):1-68.
    [3]邱正杰,范宏瑞,丛培章,等.造山型金矿床成矿过程研究进展[J].矿床地质,2015,34(1):21-38.
    [4]江思宏,聂凤军,刘翼飞.西藏马攸木金矿床的矿床类型讨论[J].矿床地质,2008,27(2):220-229.
    [5]孙晓明,熊德信,翟伟,等.云南哀牢山喜马拉雅期碰撞造山型金矿矿化机制和成矿模式[J].矿物岩石地球化学通报,2008,27(z1):52-53.
    [6]裴英茹,杨竹森,赵晓燕,等.藏北商旭金矿床S、Pb同位素组成:对成矿物质来源的指示[J].地质学报,2016,90(2):341-351.
    [7]黄瀚霄,李光明,刘波,等.藏北商旭造山型金矿床的发现及意义[J].矿床地质,2014,33(3):486-496.
    [8]肖润,李胜荣,傅璐珈,等.西藏尼玛县达查金矿床同位素地球化学研究[J].现代地质,2002,16(2):165-169.
    [9]李永灿,黄瀚霄,刘洪,等.班公湖-怒江成矿带金成矿规律及成矿作用初讨[J].沉积与特提斯地质,37(2):1-13.
    [10]潘桂棠,王立全,李荣社,等.多岛弧盆系构造模式:认识大陆地质的关键[J].沉积与特提斯地质,2012,32(3):1-20.
    [11]潘桂棠,朱弟成,王立全,等.班公湖-怒江缝合带作为冈瓦纳大陆北界的地质地球物理证据[J].地学前缘,2004,11(4):371-382.
    [12]耿全如,潘桂棠,王立全,等.班公湖-怒江带、羌塘地块特提斯演化与成矿地质背景[J].地质通报,2011,30(8):1261-1274.
    [13]潘桂棠,莫宣学,侯增谦,等.冈底斯造山带的时空结构及演化[J].岩石学报,2006,22(3):521-533.
    [14]Ding L,Lai Q.New geological evidence of crustal thickening in the Gangdise block prior to the Indo-Asian collision[J].Chinese Science Bulletin,2003,48(15):1604-1610.
    [15]曲晓明,辛洪波,杜德道,等.西藏班公湖-怒江缝合带中段碰撞后A型花岩的时代及其对洋盆闭合时间的约束[J].地球化学,2012,41(1):1-14.
    [16]Zhu D C,Zhao Z D,Niu Y L,et al.The Lhasa terrane:record of a microcontinent and its histories of drift and growth[J].Earth Planetary Science Letters,2011,301(1):241-255.
    [17]Shi R D,Yang J S,Xu Z Q,et al.The Bangong lake ophiolite(nw Tibet)and its bearing on the tectonic evolution of the Bangong-Nujiang suture zone[J].Journal of Asian Earth Sciences,2008,32(5):438-457.
    [18]王保弟,王立全,许继峰,等.班公湖-怒江结合带洞错地区舍拉玛高压麻粒岩的发现及其地质意义[J].地质通报,2015,34(9):1605-1616.
    [19]Chen Y,Zhu D C,Zhao Z D,et al.Slab breakoff triggered ca.113 Ma magmatism around Xainza area of the Lhasa Terrane,Tibet[J].Gondwana Research,2014,26(2):449-463.
    [20]唐熊,陶晓风,Tang X,等.措勤地区竟柱山组沉积特征及构造意义[J].沉积与特提斯地质,2009,29(1):53-57.
    [21]Zhu D C,Li S M,Cawood P A,et al.Assembly of the Lhasa and Qiangtang terranes in central Tibet by divergent double subduction[J].Lithos,2015,245:7-17.
    [22]雍永源.板块剪式汇聚加地体拼贴——中特提斯消亡的新模式[J].沉积与特提斯地质,2000,20(1):85-89.
    [23]邬建斌,许继峰,陈建林,等.青藏高原中部班公湖-怒江缝合带木嘎岗日群碎屑锆石年代学特征及其意义[A].2011年全国岩石学与地球动力学研讨会论文集[C].西安:中国地质学会,2011.358-359.
    [24]吕立娜,赵元艺,宋亮,等.西藏班公湖-怒江成矿带西段富铁矿与铜(金)矿C、Si、O、S和Pb同位素特征及地质意义[J].地质学报,2011,85(8):1291-1304.
    [25]雍永源.青藏高原西南部南北向构造研究的新见解[J].沉积与特提斯地质,2012,32(3):21-30.
    [26]赵文津,吴珍汉.加强地表层与深层调查的结合,深化对中国大地构造特征的认识——纪念黄汲清先生100周年诞辰[J].地质论评,2004,50(3):256-266.
    [27]唐菊兴,孙兴国,丁帅,等.西藏多龙矿集区发现浅成低温热液型铜(金银)矿床[J].地球学报,2014,35(1):6-10.
    [28]常青松,朱弟成,赵志丹,等.西藏羌塘南缘热那错早白垩世流纹岩锆石U-Pb年代学和Hf同位素及其意义[J].岩石学报,2011,27(7):2034-2044.
    [29]朱弟成,潘桂棠,莫宣学,等.冈底斯中北部晚侏罗世—早白垩世地球动力学环境:火山岩约束[J].岩石学报,2006,22(3):534-546.
    [30]黄瀚霄,龚福志,李光明,等.西藏羌塘南缘早白垩世普让岩体的锆石U-Pb年龄和地球化学特征及其地质意义[J].地质论评,2016,62(3):569-584.
    [31]刘洪,张晖,李光明,等.藏北羌塘南缘早白垩世青草山强过铝质S型花岩的成因:来自地球化学和锆石U-Pb年代学的约束[J].北京大学学报(自然科学版),2016,52(5):848-860.
    [32]朱弟成,潘桂棠,王立全,等.西藏冈底斯带中生代岩浆岩的时空分布和相关问题的讨论[J].地质通报,2008,27(9):1535-1550.
    [33]李金祥,李光明,秦克章,等.班公湖带多不杂富金斑岩铜矿床斑岩-火山岩的地球化学特征与时代:对成矿构造背景的制约[J].岩石学报,2008,24(3):531-543.
    [34]张璋,耿全如,彭智敏,等.班公湖-怒江成矿带西段材玛花岩体岩石地球化学及年代学[J].沉积与特提斯地质,2011,31(4):86-96.
    [35]廖六根,曹圣华,肖业斌,等.班公湖-怒江结合带北侧陆缘火山-岩浆弧带的厘定及其意义[J].沉积与特提斯地质,2008,28(2):163-170.
    [36]Wei S G,Tang J X,Song Y,et al.Early Cretaceous bimodal volcanism in the Duolong Cu mining district,western Tibet:Record of slab breakoff that triggered ca.108-113 Ma magmatism in the western Qiangtang terrane[J].Journal of Asian Earth Sciences,2017,138:588-607.
    [37]吴浩,李才,胡培远,等.西藏尼玛县塔色普勒地区去申拉组火山岩的发现及其地质意义[J].地质通报,2013,32(7):1014-1026.
    [38]宋扬,唐菊兴,曲晓明,等.西藏班公湖—怒江成矿带研究进展及一些新认识[J].地球科学进展,2014,29(7):795-809.
    [39]Wang Q,Zhu D C,Zhao Z D,et al.Origin of the ca.90 Ma magnesia-rich volcanic rocks in SW Nyima,central Tibet:Products of lithospheric delamination beneath the LhasaQiangtang collision zone[J].Lithos,2014,198-199(3):24-27.
    [40]王伟,曾令森,刘静,等.西藏措勤晚白垩世英安岩的厘定与地球化学特征[J].地质科学,2013,48(2):484-500.
    [41]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.
    [42]李胜荣,肖润,周肃,等.西藏改则地区金成矿作用[J].矿床地质,2005,24(1):1-14.
    [43]范建军,李才,王明,等.班公湖-怒江缝合带仲洋岛地球化学和年代学研究——兼论班公湖-怒江缝合带的闭合时限[A].全国岩石学与地球动力学研讨会[C].2012.422-423.
    [44]刘洪,李光明,黄瀚霄,等.班公湖—怒江成矿带商旭造山型金矿床Ⅲ号矿段深部找矿潜力研究[J].地质学报,2017,91(6):1245-1258.
    [45]肖万峰,李光明,黄瀚霄,等.藏北商旭金矿床控矿因素及其找矿标志[J].黄金,2013,34(10):17-21.
    [46]Kapp P,Yin A,Harrison T M,et al.Cretaceous-Tertiary shortening,basin development,and volcanism in central Tibet[J].Geological Society of America Bulletin,2005,117(7-8):865-878.
    [47]裴英茹,杨竹森,赵晓燕,等.藏北商旭金矿床成因研究:流体包裹体及氢-氧同位素证据[J].地质学报,2015,89(10):1814-1825.
    [48]肖万峰,刘洪,李光明,等.藏北双湖县商旭造山型金矿床的中低温低盐度CO2成矿流体:流体包裹体、H-O同位素的证据[J].地质论评,2017,63(3):793-808.
    [49]刘洪,黄瀚霄,李光明,等.因子分析在藏北商旭金矿床地球化学勘查中的应用[J].中国地质,2015,42(4):1126-1136.
    [50]欧阳渊,刘洪,黄瀚霄,等.藏北商旭-达则地区水系沉积物地球化学多元统计分析与找矿方向[J].矿物学报,2016(4):586-594.
    [51]肖龙.汇聚板块边缘的金矿成矿作用[J].地质科技情报,2000,19(1):46-50.
    [52]陈顺.西藏班公湖-怒江带西段改则地区木嘎岗日岩群物质组成及构造意义[D].成都:成都理工大学,2015.1-100.
    [53]曹圣华,邓世权,肖志坚,等.班公湖-怒江结合带西段中特提斯多岛弧构造演化[J].沉积与特提斯地质,2006,26(4):25-32.

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