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    新疆金坝金矿成矿作用的地质和流体包裹体证据

    王颖维 徐九华 卫晓锋 丁汝福

    王颖维, 徐九华, 卫晓锋, 丁汝福, 2018. 新疆金坝金矿成矿作用的地质和流体包裹体证据. 地球科学, 43(9): 3112-3125. doi: 10.3799/dqkx.2018.159
    引用本文: 王颖维, 徐九华, 卫晓锋, 丁汝福, 2018. 新疆金坝金矿成矿作用的地质和流体包裹体证据. 地球科学, 43(9): 3112-3125. doi: 10.3799/dqkx.2018.159
    Wang Yingwei, Xu Jiuhua, Wei Xiaofeng, Ding Rufu, 2018. The Mineralization of the Jinba Gold Deposit, Xinjiang, China: Evidence from Geology and Fluid Inclusions. Earth Science, 43(9): 3112-3125. doi: 10.3799/dqkx.2018.159
    Citation: Wang Yingwei, Xu Jiuhua, Wei Xiaofeng, Ding Rufu, 2018. The Mineralization of the Jinba Gold Deposit, Xinjiang, China: Evidence from Geology and Fluid Inclusions. Earth Science, 43(9): 3112-3125. doi: 10.3799/dqkx.2018.159

    新疆金坝金矿成矿作用的地质和流体包裹体证据

    doi: 10.3799/dqkx.2018.159
    基金项目: 

    国家自然科学基金项目 41372096

    国家重点基础研究发展计划(973计划)项目 2014CB440803

    国家自然科学基金项目 41672070

    详细信息
      作者简介:

      王颖维(1991-), 女, 博士, 主要从事矿床学研究方向

    • 中图分类号: P618

    The Mineralization of the Jinba Gold Deposit, Xinjiang, China: Evidence from Geology and Fluid Inclusions

    • 摘要: 金坝金矿作为额尔齐斯构造成矿带的典型金矿,人们对其构造蚀变特征、成矿流体演化以及成矿热液来源还缺乏深入研究,区内岩浆活动与金坝金矿之间的关系尚不明确.在矿床地质特征研究基础上,详细分析矿化蚀变特征,使用扫描电镜阴极发光(SEM-CL)分析石英显微结构,通过流体包裹体研究和S-D-O同位素分析对成矿流体和矿质来源进行探讨.区内黄铁矿化、绢云母化、硅化普遍发育,是重要的找矿标志.矿区斜长花岗岩和闪长岩的钻孔样品由矿化中心向外蚀变及矿化逐渐减弱,变化明显.SEM-CL显示石英微结构具有热液石英特征的穿插结构和重结晶结构,表明变形变质作用强烈.热液成矿分为4个阶段:磁铁矿-石英阶段、金-黄铁矿-石英阶段、金-多金属硫化物-石英阶段和石英-碳酸盐化阶段.金坝金矿的流体包裹体多以水溶液包裹体为主,并有CO2-H2O包裹体及碳质流体包裹体.成矿温度主峰为260~280 ℃和380~400 ℃,盐度范围在0.88%~13.72% Nacleqv,流体密度为0.90~0.95 g/cm3.表明成矿流体体系为中高温热液、中低盐度、中低密度的H2O-NaCl-CO2体系.成矿流体有从中高温富CO2向低温盐水溶液演化的特点.矿床硫质来源具有深源硫特征.流体包裹体中δDH2O值为-78.0‰~-80.5‰,成矿溶液的δ18OH2O值为1.49‰~5.31‰,表明成矿热液流体由成矿早期的岩浆水向晚期成矿流体的大气降水演化.

       

    • 图  1  新疆金坝金矿区域地质简图

      Fig.  1.  Geological sketch of Jinba gold deposit in Xinjiang

      图  2  金坝金矿矿区平面图

      图据正元国际矿业有限公司内部资料(2012)

      Fig.  2.  Geological sketch of Jinba gold deposit

      图  3  金坝金矿蚀变岩石钻孔岩心特征

      a.闪长岩脉型矿石,浸染状黄铁矿化,ZK15-2-282;b.糜棱岩化斜长花岗岩,石英呈眼球状、透镜状分布,构造挤压强烈,ZK15-2-120;c.斜长花岗质碎裂岩,绿帘石发育,ZK15-2-130.5;d.蚀变带内斜长花岗岩,碎斑角砾拉长,ZK15-2-150;Py.黄铁矿;Ep.绿帘石;Qtz.石英

      Fig.  3.  Photos showing the drill core features of altered rock of Jinba gold deposit

      图  4  金坝金矿区15勘探线剖面

      图据正元国际矿业有限公司内部资料(2010)

      Fig.  4.  Section plan of line 15 in Jinba gold deposit

      图  5  金坝金矿围岩、矿石显微镜下特征

      a.碎斑状石英裂隙晚期石英细脉充填,样品号:ZK15-2-190,(正交光);b.弱蚀变斜长花岗岩,黑云母化,样品号:ZK15-2-190(正交光);c.蚀变较强的绿泥石化黝帘石化碎裂斜长花岗岩,ZK15-2-176(正交光);d.绿泥石化黝帘石化,达到糜棱岩化斜长花岗岩,黝帘石深蓝色干涉色明显,样品号:ZK15-2-127(正交光);e.辉长闪长岩中黄铁矿-石英细脉,样品号:ZK15-1-280(单偏光);f.闪长岩型矿石,浸染状黄铁矿黄铜矿,样品号:ZK15-1-282(反光);Q.石英;Bt.黑云母;Chl.绿泥石;Zo.黝帘石;Py.黄铁矿;Ccp.黄铁矿

      Fig.  5.  Photos showing the microscopic characteristics of surrounding rock and ore in Jinba gold deposit

      图  6  石英SEM-CL图像

      a.浅色CL石英被可代表破裂的暗色CL石英分隔而呈块状;b.浅色CL石英被可代表破裂的暗色CL石英分隔而呈块状,受构造作用浅色CL石英沿线性方向生长;c.浅色CL石英被宽大的灰色CL石英边包裹,未完全包裹;d.石英颗粒内具有暗色CL核部

      Fig.  6.  Quartz SEM-CL image

      图  7  金坝金矿流体包裹体显微特征

      a.闪长岩中黄铁矿石英脉,变形弱,L-V及包裹体群,ZK8-3-270;b.斜长花岗岩中透镜状石英L-V包裹体群,ZK15-2-117;c.变形斜长花岗岩中残留的透镜状石英内L-V与富二氧化碳包裹体群共存,ZK15-2-117;d.闪长岩中黄铁矿石英脉,碳质包裹体,ZK8-3-270

      Fig.  7.  Microscopic characteristics of fluid inclusions of Jinba gold deposit

      图  8  流体包裹体均一温度柱状图

      本次实验测试包裹体74个

      Fig.  8.  Histogram of homogenization temperature of fluid inclusions

      图  9  金坝金矿包裹体激光拉曼探针图谱分析结果

      a.ZK15-2-117-7(水溶液包裹体-液相);b.ZK15-2-117-13(碳质包裹体-气相);c.ZK15-2-117-5(富CO2包裹体-液相);d.ZK8-3-255.5-5(富CO2三相包裹体-气相).图中包裹体大小为10~12 μm

      Fig.  9.  Analytical results of laser Raman probe of the fluid inclusions in Jinba gold deposit

      图  10  金坝金矿包裹体中δD-δ18O关系

      Fig.  10.  Diagram of δD-δ18O for fluid inclusion of Jinba gold deposit

      图  11  硫同位素组成

      赛都金矿硫同位素数据据程忠富和芮行健(1997)张国瑞(2007)

      Fig.  11.  Histogtam of sulfur isotope compositions of sulfides

      表  1  金坝金矿区15勘探线构造蚀变带岩性特征

      Table  1.   Lithologic characteristics of structural alteration zone of line 15 in Jinba gold deposit

      钻孔 样号 岩性 野外、镜下特征
      ZK15-2 JB-ZK15-2-062 弱蚀变斜长花岗岩 斜长石(60%)发生黝帘石化,石英30%,包括透镜状石英及其周边重结晶亚颗粒石英.
      JB-ZK15-2-107 弱蚀变斜长花岗岩 斜长石(50%)见微斜长石,石英(30%),网脉状硅化、绿帘石化,镜下绢云母化,脉状绿泥石化.
      JB-ZK15-2-108 碎裂斜长花岗岩 碎斑为角砾状石英(动力变质作用),石英(35%),斜长石(55%)大多被交代,黝帘石化、绢云母化强烈.
      JB-ZK15-2-114 绿泥石化斜长花岗岩 斜长石(30%),石英(30%),绿帘石(15%),绿泥石化、绿帘石化明显(镜下异常干涉色).
      JB-ZK15-2-116 绿泥石化斜长花岗岩 斜长石(60%),石英(20%),透镜状石英及其周边重结晶亚颗粒石英发育,糜棱岩化.
      JB-ZK15-2-117 糜棱岩化斜长花岗岩 斜长石(60%),石英(20%),构造-蚀变强烈,镜下透镜状石英及其周边重结晶亚颗粒石英发育,绢云母化强.
      JB-ZK15-2-120 糜棱岩化斜长花岗岩 同上,构造挤压强烈,糜棱岩化发育,角砾状透镜状石英.
      JB-ZK15-2-125 糜棱岩化斜长花岗岩 斜长石(60%),石英(30%),镜下绿泥石化、黝帘石化强烈.
      JB-ZK15-2-127 糜棱岩化斜长花岗岩 斜长石(60%),石英(30%),糜棱岩化,镜下绿泥石化、黝帘石化、碳酸盐化强烈.
      JB-ZK15-2-130 碎裂斜长花岗岩 碎斑石英(角砾状石英)发育,绿帘石化强烈.
      JB-ZK15-2-137 碎裂斜长花岗岩 斜长石(65%),石英(35%),石英变形强烈,见较多的次生包裹体和残留的原生包裹体.
      JB-ZK15-2-146 绿泥石化斜长花岗岩 斜长石(60%),石英(20%),角闪石(10%),流动构造强烈,镜下绿泥石化、绢云母化.
      JB-ZK15-2-176 碎裂斜长花岗岩 斜长石(65%),石英(20%),糜棱岩化发育,绿帘石化、绿泥石化.
      JB-ZK15-2-190 弱蚀变斜长花岗岩 斜长石(55%),见微斜长石,石英(35%),绿泥石化.
      ZK15-1 JB-ZK15-1-279 辉长闪长岩 角闪石含量>65%,斜长石(30%),见星点状黄铁矿.
      JB-ZK15-1-280 蚀变闪长岩 斜长石(40%),绿帘石(30%),角闪石(10%),绿帘石化发育,见星点状、长条状黄铁矿.
      JB-ZK15-1-282 闪长岩型矿石 斜长石(50%),角闪石(15%),黑云母(20%),浸染状黄铁矿化,见黄铜矿化,透闪石化、绿泥石化、绿帘石化强.
      JB-ZK15-1-283 蚀变斜长花岗岩 斜长石(50%),角闪石(10%),石英(20%),绿泥石(15%),白云母(绢云母)化、绿泥石化、绿帘石化.
      JB-ZK15-1-348 碎裂斜长花岗岩 斜长石(60%),石英(35%),糜棱岩化发育.
      JB-ZK15-1-351 蚀变辉长闪长岩 斜长石(40%),石英(30%),角闪石(30%),角闪石具定向构造,磁铁矿定向排列.
      JB-ZK15-1-357 蚀变辉长闪长岩 斜长石(50%),石英(20%), 绿泥石(20%),接触带,硅化、石英脉、黄铁矿化.
      JB-ZK15-1-365 蚀变辉长闪长岩 角闪石含量>50%,斜长石(30%),角闪石柱状变晶,磁铁矿沿角闪石边部析出,定向排列.
      注:JB-ZK15-2-062样号表示15号勘探线15-2钻孔62 m处.
      下载: 导出CSV

      表  2  新疆哈巴河县金坝金矿流体包裹体显微测温综合分析

      Table  2.   Comprehensive analysis of microtemperature measurement of fluid inclusion of Jinba gold deposit in Habahe County, Xinjiang

      样品号 采样位置 成矿阶段 样品特征 包裹体类型 大小(μm) Th, tot(℃) Tm, ice(℃) 盐度(% NaCleqv) Tm, CO2(℃) Th, CO2(℃) 产出特点
      8-3-255.5 ZK8-3-255.5 主成矿阶段 斜长花岗岩中透镜状石英 LH2O-VH2O 2~12 254~280(4) RD, M
      LCO2-LH2O 4~8 247~258(13) -56.9~-57.8(6) 29.4~30.4(9) RD, B
      8-3-270 ZK8-3-270 主成矿阶段 闪长岩中浸染状黄铁矿石英脉 LH2O-VH2O 4~12 -2.3~-2.6(6) 3.71~4.34(6) RD, C
      8-3-273 ZK8-3-273 主成矿阶段 斜长花岗岩中石英脉 LH2O-VH2O 2~12 200~220(4) -4.4~-7.7(7) 7.02~11.34(7) RD, C
      LCO2-LH2O 4~12 -60.4~-56.9(4) 12.2~30.9(4) RD
      15-2-117 ZK15-2-117 成矿早阶段 斜长花岗岩中透镜状石英 LH2O-VH2O 4~20 265~396(31) -0.5~-9.8(13) 0.88~13.72(13) B, C
      LCO2-LH2O 4~16 262~401(22) -60.4~-57.1(9) 15.3~30.6(10) I, B, C
      LCO2 4~8 B, C
        注:I.孤立分布;RD.随机无序包裹体群;B.带状包裹体群;C.簇状包裹体群;M.串珠状包裹体群;括号内数字为测试个数.
      下载: 导出CSV

      表  3  金坝金矿的黄铁矿硫同位素组成

      Table  3.   Sulfur isotopic composition of pyrite of Jinba gold deposit

      样品号 岩石名称 δ34SV-CDT(‰) 备注
      DJ15-1 蚀变辉长闪长岩中的浸染状黄铁矿 6.89 中国科学院地球化学研究所环境地球化学国家重点实验室测试
      DJ15-2 8.71
      DJ15-2 8.33
      DJ15-3 7.98
      DJ15-4 3.75
      DJ15-4 3.42
      DJ15-7 5.00
      ZK-15-1-282 闪长岩型矿石中浸染状黄铁矿 8.70 中国科学院地质与地球物理研究所岩石圈演化国家重点实验室稳定同位素实验室测试
      下载: 导出CSV

      表  4  金坝金矿石英流体包裹体氢、氧同位素组成

      Table  4.   Hydrogen and oxygen composition in fluid inclusions from the Jinba gold deposit

      样品编号 对应成矿阶段 校正后温度(℃) δ18O(‰) δ18OH2O(‰) δDH2O(‰)
      ZK-15-2-177 成矿早阶段 400 9.4 4.81 -78.00
      ZK-15-2-177 400 9.7 5.11 -78.20
      ZK-15-2-177 400 9.9 5.31 -78.50
      ZK-8-3-48.5 主成矿阶段 280 10.7 1.99 -80.00
      ZK-8-3-48.5 280 10.2 1.49 -80.50
      下载: 导出CSV

      表  5  金坝金矿与邻近金矿的地质特征对比

      Table  5.   Table of characteristics of ore forming fluid of Jinba gold deposit, Saidu gold deposit and Axile gold deposit

      矿床 含矿地层 赋矿岩石 控矿构造 矿区内侵入岩 矿石建造 围岩蚀变 成矿阶段 成矿流体特征
      阿希勒金矿 中泥盆统托克萨雷组(D1-2) 石英闪长岩、糜棱岩 额尔齐斯次级构造带-阿希勒断裂以及玛尔卡库里断裂带 斜长花岗岩、英云闪长岩、花岗闪长岩和辉长闪长岩 石英-金-黄铁矿-硫化物 硅化、黄铁矿化、绢云母化、绿泥石化及孔雀石化 Ⅰ.早期白色石英脉阶段;Ⅱ.贫硫化物石英脉阶段;Ⅲ.浸染状黄铁矿化石英脉阶段 包裹体类型:①富CO2包裹体;②水溶液包裹体;③纯H2O的单相包裹体;均一温度:中-低温125.2~298.7 ℃,低盐度0.35%~10%,低密度,热液主要来源于岩浆水并有围岩中水的参与.
      赛都金矿 中下泥盆统托克萨雷组(D1-2) 含金石英脉、蚀变千枚岩、闪长岩、斜长花岗斑岩 玛尔卡库里韧性剪切带及其原生的托库孜巴依次级韧性剪切带 闪长岩脉和斜长花岗斑岩脉 石英-绢云母-碲矿物-硫化物-金 硅化、钾化、钠长石化、绢云母化、黄铁矿化、次生石英化、绿泥石化及碳酸盐化 Ⅰ.早期硅化阶段;Ⅱ.浸染状黄铁矿-乳白色石英阶段;Ⅲ.多金属硫化物-烟灰色石英阶段;Ⅳ.晚期石英-碳酸盐化阶段 包裹体类型:①水溶液包裹体;②富N2包裹体和CO2包裹体;③CO2-H2O包裹体;中低温100~300 ℃;中低盐度0.35%~9.86%,低密度,热液主要来自于岩浆水,在金矿的形成过程中有围岩水的参与。由成矿早期的岩浆水向晚期成矿流体的大气降水演化.
      金坝金矿 中泥盆阿舍勒组(D1-2 αs) 斜长花岗岩、闪长岩、含金石英脉、绢云绿泥千枚岩和黄铁矿化石英砂岩 玛尔卡库里大断裂早期韧性剪切以及区内次一级北西-南东向脆性断裂构造 斑状斜长花岗岩、中粗粒斜长花岗岩、混染岩化斜长花岗岩、斜长岩脉和闪长岩脉 石英-金-黄铁矿-硫化物 绢云母化、绿泥石化、硅化、黄铁矿化、黝帘石化、绿帘石化及绿泥石化 Ⅰ.磁铁矿-石英阶段;Ⅱ.金-黄铁矿-石英阶段;Ⅲ.金-多金属硫化物-石英阶段;Ⅳ.石英-碳酸盐阶段 包裹体类型:①水溶液包裹体;②CO2-H2O包裹体;③碳质流体包裹体;中高温200~400 ℃,中低盐度0.88%~13.72%,低密度,热液来源:成矿流体由成矿早期的岩浆水向晚期成矿流体的大气降水演化.
        注:据单立华(2008)卫晓峰等(2011)张国瑞(2007)徐九华等(2009)整理.
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