[an error occurred while processing this directive] 世界地质 2018, 37(4) 1058-1067 DOI:   10.3969/j.issn.1004-5589.2018.04.006  ISSN: 1004-5589 CN: 22-1111/P

本期目录 | 下期目录 | 过刊浏览 | 高级检索                                                            [打印本页]   [关闭]
基础地质
扩展功能
本文信息
Supporting info
PDF(888KB)
[HTML全文]
参考文献[PDF]
参考文献
服务与反馈
把本文推荐给朋友
加入我的书架
加入引用管理器
引用本文
Email Alert
文章反馈
浏览反馈信息
本文关键词相关文章
卓玛铜铅锌矿床
流体包裹体
云南
本文作者相关文章
江海洋
马雪俐
高明波
王可勇
杨贺
PubMed
Article by Jiang H
Article by Ma X
Article by Gao M
Article by Wang K
Article by Yang H
滇西北卓玛Cu-Pb-Zn矿床成矿流体特征
江海洋1,2, 马雪俐1, 高明波2, 王可勇1, 杨贺1
1. 吉林大学地球科学学院, 长春 130061;
2. 山东省第一地质矿产勘查院, 济南 250014
摘要: 卓玛矿床位于云南香格里拉格咱弧东北部,属斑岩-热液脉型铜多金属矿床。矿体主要赋存于矿区石英二长斑岩内及附近,严格受NW向断裂控制。卓玛矿床的形成经历了黄铁矿-石英(Ⅰ)、黄铁矿±黄铜矿-石英(Ⅱ)、黄铁矿±黄铜矿±方铅矿±闪锌矿-石英(Ⅲ)及贫硫化物-石英-碳酸盐(Ⅳ)四个成矿阶段。通过对各成矿阶段研究样品石英颗粒中的原生流体包裹体进行岩相学、显微测温学及激光拉曼光谱研究,探讨卓玛铜多金属矿床成矿流体特征,结果表明:Ⅰ阶段石英中主要发育富CO2及气液两相型包裹体;Ⅱ阶段石英中主要发育碳质、富CO2、含CO2及气液两相4种类型包裹体;Ⅲ阶段石英中主要发育含CO2及气液两相型包裹体;Ⅳ阶段石英中主要发育富CO2、含CO2及气液两相3种类型包裹体。激光拉曼光谱显示碳质包裹体主要成分为CO2和CH4,而CO2包裹体中除CO2和CH4气相成分外,还有部分H2O。因此,综合研究结果显示卓玛铜多金属矿床成矿流体为中温、低盐度的CO2-CH4-NaCl-H2O体系热液。成矿过程中,流体温度和盐度数值略有降低趋势,成矿流体的不混溶作用是导致成矿物质大量卸载的关键因素。
关键词 卓玛铜铅锌矿床   流体包裹体   云南  
Characteristics of fluid inclusions of Zhuoma Cu-Pb-Zn deposit, northwestern Yunnan
JIANG Hai-yang1,2, MA Xue-li1, GAO Ming-bo2, WANG Ke-yong1, YANG He1
1. College of Earth Sciences, Jilin University, Changchun 130061, China;
2. No.1 Institute of Geology and Mineral Resources of Shandong Province, Jinan 250014, China
Abstract: Zhuoma Cu-Pb-Zn deposit, located in northeastern Garze arc,Shangrila,Yunnan Province, is a porphyry-hydrothermal vein-type deposit. Ore bodies are mainly hosted in quartz monzonite porphyry and controlled by NW-trending faults. Cu polymetallic mineralization in this deposit consists of four stages of paragenesis, namely (Ⅰ) pyrite-quart, (Ⅱ) pyrite ±chalcopyrite-quartz, (Ⅲ) pyrite ±chalcopyrite ±galena ±sphalerite-quartz and (Ⅳ) barren sulfide-quartz-carbonate. The comprehensive study on petrography, microthermometry and laser Raman of fluid inclusions showed that:CO2-rich and liquid-rich fluid inclusions were observed in stage Ⅰ; C-type, CO2-rich, CO2-bearing and liquid-rich fluid inclusions were observed in stage Ⅱ; only CO2-bearing and liquid-rich fluid inclusions were observed in stage Ⅲ; CO2-rich, CO2-bearing and liquid-rich fluid inclusions were observed in stage Ⅳ. Laser Raman spectrum suggest that the main components of C-type inclusions are CO2 and CH4, while in CO2 inclusions, there are some H2O in addition to CO2 and CH4 in gas phase. Comprehensive research indicates that the ore-forming fluids in Zhuoma deposit are characterized by a medium temperature, low salinity CO2-CH4-NaCl-H2O system of hydrothermal fluids, and the immiscibility of fluids is a key factor leading to the discharging of minerals in mineralization.
Keywords: Zhuoma Cu-Pb-Zn deposit   fluid inclusion   Yunnan  
收稿日期 2018-07-07 修回日期 2018-10-25 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2018.04.006
基金项目:

国家"973"计划项目(2009CB421007).

通讯作者: 马雪俐(1993-),女,博士研究生,主要从事地质矿床学研究.E-mail:2269548350@qq.com
作者简介:
作者Email: 2269548350@qq.com

参考文献:
[1] 李文昌, 尹光侯, 余海军, 等. 滇西北格咱火山-岩浆弧斑岩成矿作用[J]. 岩石学报, 2011, 27(9):2541-2552. LI Wen-chang, YIN Guang-hou, YU Hai-jun, et al. The porphyry metallogenesis of Geza volcanic magmatic arc in NW Yunnan[J]. Acta Petrologica Sinica, 2011,27(9):2541-2552.
[2] 曾普胜, 莫宣学, 喻学惠, 等. 滇西北中甸地区中-酸性斑岩及其含矿性初步研究[J]. 地球学报, 1999, 20(增刊):359-364. ZENG Pu-sheng, MO Xuan-xue, YU Xue-hui, et al. Preliminary research on the intermediate-acidic porphyries and their ore-bearing in the Zhongdian area, Northwest Yunnan[J]. Acta Geoscientia Sinica, 1999, 20(Suppl.):359-364.
[3] 曾普胜, 莫宣学, 喻学惠, 等. 滇西北中甸斑岩及斑岩铜矿[J]. 矿床地质, 2003, 22(4):393-400. ZENG Pu-sheng, MO Xuan-xue, YU Xue-hui, et al. Porphyries and porphyry copper deposits in Zhongdian area, northwestern Yunnan[J].Mineral Deposits, 2003, 22(4):393-400.
[4] 李文昌, 尹光侯, 余海军, 等. 滇西北格咱火山-岩浆弧斑岩成矿作用[J]. 岩石学报, 2011, 27(9):2541-2552. LI Wen-chang, YIN Guang-hou, YU Hai-jun, et al. The porphyry metallogenesis of Geza volcanic magmatic arc in NW Yunnan[J]. Acta Petrologica Sinica, 2011, 27(9):2541-2552.
[5] 李建康, 李文昌, 王登红, 等.中甸弧燕山晚期成矿事件的Re-Os定年及成矿规律研究[J]. 岩石学报,2007,23(10):2415-2422. LI Jian-kang, LI Wen-chang, WANG Deng-hong, et al. Re-Os dating for ore-forming event in the late of Yanshan Epoch and research of ore-forming regularity in Zhongdian Arc[J]. Acta Petrologica Sinica, 2007, 23(10):2415-2422.
[6] 杨岳清, 侯增谦, 黄典豪, 等. 中甸弧碰撞造山作用和岩浆成矿系统[J]. 地球学报, 2002, 23(1):17-24. YANG Yue-qing, HOU Zeng-qian, HUANG Dian-hao, et al. Collision orogenic process and magmatic metallogenic system in Zhongdian arc[J]. Acta Geoscientia Sinica, 2002, 23(1):17-24.
[7] 刘学龙, 李文昌, 张娜, 等. 西南三江义敦岛弧南端地壳抬升历史及资源评价意义[J]. 地质学报, 2015, 89(2):289-304. LIU Xue-long, LI Wen-chang, ZHANG Na, et al. The crustal uplift history of the southern tip of Yidun island Arc in Southwest Sanjiang region and significance of resource evaluation[J]. Acta Geologica Sinica, 2015, 89(2):289-304.
[8] 李冰, 张世权, 胡清华, 等. 香格里拉卓玛铜铅锌多金属矿特征与资源潜力[J]. 云南地质, 2012, 31(3):331-334. LI Bing, ZHANG Shi-quan, HU Qing-hua, et al. The characteristics and potentiality of Zhuoma Cu-Pb-Zn multimetallic deposit, Xianggelila[J]. Yunnan Geology, 2012, 31(3):331-334.
[9] 金灿海, 范文玉, 张海, 等. 云南卓玛铅锌矿床地球化学特征及矿床成因[J]. 中国地质, 2013, 40(6):1902-1911. JIN Can-hai, FAN Wen-yu, ZHANG Hai, et al. Geochemical characteristics and genesis of the Zhuoma lead-zinc deposit in Yunnan Province[J]. Geology in China, 2013, 40(6):1902-1911.
[10] 刘学龙,李文昌,张娜. 云南卓玛成矿斑岩体锆石U-Pb年龄及地球化学特征[J]. 矿物岩石地球化学通报, 2016, 35(1):109-117. LIU Xue-long, LI Wen-chang, ZHANG Na. Zircon U-Pb age and geochemical characteristics of the quartz monzonite porphyry from the Zhuoma deposit, Yunnan, China[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2016, 35(1):109-117.
[11] 李剑锋, 林文昌, 尹光候, 等.滇西北卓玛铜多金属矿床成矿流体特征研究[J]. 吉林大学学报(地球科学版), 2015, 45(增刊1):1-2. LI Jian-feng, LIN Wen-chang, YIN Guang-hou, et al. Characteristics of ore-forming fluid of Zhuma copper polymetallic deposit in northwestern Yunnan[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(Suppl.1):1-2
[12] 张兴春, 秦朝建, 王守旭, 等.云南中甸卓玛铜-多金属矿床地质特征及流体包裹体初步研究[J]. 矿物岩石地球化学通报, 2004, 23(增刊):103. ZHANG Xing-chun, QIN Chao-jian, WANG Shou-xu, et al. Geological characteristics and fluid inclusions of the Zhuma copper polymetallic deposit in Zhongdian, Yunnan[J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2004, 23(Suppl.):103.
[13] 李文昌, 王可勇, 尹光侯, 等. 滇西北红山铜矿床成矿流体地球化学特征及矿床成因[J]. 岩石学报, 2013, 29(1):270-282. LI Wen-chang, WANG Ke-yong, YIN Guang-hou, et al. Geochemical characteristics of ore-forming fluids and genesis of Hongshan copper deposit in northwestern Yunnan Province[J]. Acta Petrologica Sinica, 2013, 29(1):270-282.
[14] Brown P E, Hagemann S G. MacFlincor and its application to fluids in Archean lode-gold deposits[J].Geochimica et Cosmochimica Acta, 1995,59(19):3943-3952.
[15] Roedder E. Fluid inclusions:reviews in mineralogy[M].Washington:Mineralogical Society of American, 1984:1-644.
[16] 张德会. 流体的沸腾和混合在热液成矿中的意义[J]. 地球科学进展, 1997, 12(6):546-552. ZHANG De-hui. Some new advances in ore-forming fluid geochemistry on boiling and mixing of fluids during the processes of hydrothermal deposits[J]. Advances in Earth Science, 1997, 12(6):546-552.
[17] Drummond S E, Ohmoto H.Chemical evolution and mineral deposition in boiling hydrothermal systems[J].Economic Geology, 1985,80(1):126-147.
[18] MAO Wei, Brian R, YANG Fu-chu, et al. Physical and chemical evolution of the Dabaoshan porphyry Mo deposit, South China:insights from fluid inclusions, cathodoluminescence, and trace elements in quartz[J]. Economic Geology, 2017, 112:889-918.
[19] 刘翼飞, 聂凤军, 江思宏, 等. 内蒙古查干花钼矿床成矿流体特征及矿床成因[J]. 吉林大学学报(地球科学版), 2011, 41(6):1794-1805. LIU Yi-fei, NIE Feng-jun, JIANG Si-hong, et al. Ore-forming fluid characteristics and ore genesis of Chaganhua porphyry molybdenum deposit in central Inner Mongolia, China[J]. Journal of Jilin University(Earth Science Edition), 2011, 41(6):1794-1805.
[20] 杨志强, 吴邦友, 郑松森, 等. 新疆东戈壁斑岩型钼矿床成矿流体包裹体温度-压力研究[J]. 地质找矿论丛, 2012, 27(3):308-314. YANG Zhi-qiang, WU Bang-you, ZHENG Song-sen, et al. Analysis of metallogenic conitions of East Gobi porphyry molybdenum deposit[J]. Contributions to Geology and Mineral Resources Research, 2012, 27(3):308-314.
[21] 王承阳, 李文昌, 王可勇, 等.滇西北雪鸡坪铜矿床流体包裹体特征研究及矿床成因讨论[J]. 岩石学报, 2015, 31(4):967-978. WANG Cheng-yang, LI Wen-chang, WANG Ke-yong, et al. Characteristics of fluid inclusions and genesis of Xuejiping copper deposit in northwestern Yunnan Province[J]. Acta Petrologica Sinica, 2015, 31(4):967-978.
[22] 李文昌, 尹光侯, 余海军, 等.云南普朗斑岩型铜矿床成矿流体特征及矿床成因[J]. 吉林大学学报(地球科学版), 2013, 43(5):1437-1447. LI Wen-chang, YIN Guang-hou, YU Hai-jun, et al. Characteristics of the fluid inclusions and genesis of the Pulang copper deposit in Yunnan Province[J]. Journal of Jilin University (Earth Science Edition), 2013, 43(5):1437-1447.
[23] 王守旭, 张兴春, 秦朝建, 等. 滇西北中甸普朗斑岩铜矿流体包裹体初步研究[J]. 地球化学, 2007, 36(5):467-478. WANG Shou-xu, ZHANG Xing-chun, QIN Chao-jian, et al. Fluid inclusions in quartz veins of Pulang porphyry copper deposit, Zhongdian, northwestern Yunnan, China[J]. Geochimica, 2007, 36(5):467-478.
[24] Roedder E, Bodnar R J. Geologic pressure determinations from fluid inclusion studies[J].Annual Review of Earth and Planetary Sciences,1980,8:263-301.
本刊中的类似文章
1.崔启杰,王可勇,李建国,马雪俐,赵华雷,杨贺,孙丽雪.松辽盆地钱家店砂岩型铀矿床油气运移与铀成矿的关系:来自流体包裹体的证据[J]. 世界地质, 2022,41(1): 92-107
2.王旭东,张东亮,卢克豪,张腾飞.黑钨矿中流体包裹体红外显微测温技术方法探讨[J]. 世界地质, 2021,40(4): 872-880
3.王焕鑫,孙丰月,张涛,闫佳铭,刘承先.青海东昆仑德里特萤石矿成因探讨:来自流体包裹体和稳定同位素的证据[J]. 世界地质, 2021,40(4): 807-815
4.刘禹铭,孙景贵,李雪梅,松权衡,王清海,张笑天. 吉林敦化松江河金矿地质、流体包裹体特征与成因研究[J]. 世界地质, 2021,40(2): 273-287
5.陆胜, 王可勇, 张涵远, 赵焕利, 相雷, 刘阳, 张志博.黑龙江漠河推覆带前哨林场锑金矿床流体包裹体特征及其地质意义[J]. 世界地质, 2020,39(3): 557-568
6.雷凤至, 孙景贵, 徐智涛, 韩吉龙, 刘阳.福建德化地区东洋浅成热液金矿床成矿作用与成因研究[J]. 世界地质, 2019,38(2): 339-353
7.徐怡然, 丁振举.湘西头坡脑汞锌矿成矿流体特征及地质意义[J]. 世界地质, 2018,37(1): 124-139
8.赵璇,任云生,郝宇杰,陈聪,商青青,李晨辉.延边地区石井金银矿床成矿流体特征及矿床成因[J]. 世界地质, 2017,36(4): 1133-1143
9.王春光,孙国胜,何欣,王广伟,任利明,李晓朋,张富胤,董晓健.内蒙古翁牛特旗硐子铅锌矿床成矿流体性质与成因[J]. 世界地质, 2017,36(4): 1116-1123
10.唐臣, 张馨文, 孙景贵.黑龙江宁安英城子金矿床的地质、流体包裹体特征与成因研究[J]. 世界地质, 2017,36(3): 826-835
11.田力丹, 孙丰月, 王力, 刘金龙, 吴琼.吉林临江荒沟山铅锌矿床流体包裹体特征及矿床成因[J]. 世界地质, 2017,36(3): 836-849
12.任军博, 杨思宇, 苏涛, 臧利斌, 全成.云南先峰中新世木乃伊化木化石α-纤维素的提取[J]. 世界地质, 2017,36(3): 1001-1007
13.张庆飞, 郭巍, 丁鸿儒, 李文强, 杨绪海, 张丛, 刘孟骐.鸡西盆地下白垩统城子河—穆棱组油气藏成藏期次研究[J]. 世界地质, 2017,36(2): 552-559,569
14.刘大中, 郝宇杰, 杨群, 赵书跃, 任云生.大兴安岭中北段古中公路钼矿床形成时代与矿床成因[J]. 世界地质, 2017,36(2): 507-519
15.权鸿雁, 蔡文艳, 张雪冰, 付丽娟, 王可勇.内蒙古维拉斯托铅锌矿床流体包裹体特征及矿床成因研究[J]. 世界地质, 2017,36(1): 105-117

Copyright by 世界地质