Cd contents and Zn/Cd Ratios of Sphalerites and Their Geological Implications
-
摘要: 以5个典型铅锌矿床为研究对象,测试了其闪锌矿中的Zn和Cd含量,发现同一标本上深色闪锌矿比晚期的浅色闪锌矿更富集Cd,其原因可能与流体中Zn/Cd值变化相关;而对比不同矿床不同颜色闪锌矿之间Cd的富集规律是没有意义的。同时,与岩浆作用相关的铅锌矿床,其闪锌矿中的Zn/Cd值与相关岩浆岩的Zn/Cd值相似,暗示闪锌矿中的Zn/Cd值可指示成矿物质来源。同时,川滇黔地区铅锌矿床显示出2组不同的Zn/Cd值:①高Zn/Cd值型(300~800),以会泽矿床为代表,其Zn/Cd值介于峨眉山玄武岩和该区地层之间,暗示该类型矿床的成矿物质可能主要来源于峨眉山玄武岩和地层。②低Zn/Cd值型(20~70),以富乐矿床为代表,其Zn/Cd值基本与地层相似,暗示该矿床的成矿物质可能主要来源于地层。而对比川滇黔地区铅锌矿床和与岩浆作用相关矿床的Cd含量及Zn/C值发现,成因不同的矿床,其Cd含量和Zn/Cd值具有较大差异。因此,铅锌矿床闪锌矿中的Cd含量及Zn/Cd值对于判别成矿物质来源和矿床成因具有指示意义。Abstract: In this paper, the Zn and Cd contents in sphalerites from five typical Zn-Pb depositshave been investigated and tested. The results show that dark sphalerite (early stage) has higher Cd contents than light one (late stage) in a hand specimen, which may be caused by Zn/Cd decreasing of ore-forming fluids. Meanwhile, the sphalerites from magma-related Zn-Pb deposits have similar Zn/Cd ratios with the source bed, suggesting that Zn/Cd ratios could be a proxy to trace the origins of metallogenic materials. Zn/Cd ratios in sphalerite from major Zn-Pb deposits in Sichuan-Yunnan-Guizhou metallogenic province could be divided into two groups, which are:①High Zn/Cd ratios (e.g. the Huize deposit), the deposits of this group have high Zn/Cd ratios (300-800),which are varied between the ones of the Emeishan basalts (Zn/Cd ratios higher than 1000) and sedimentary rocks (Zn/Cd ratios lower than 100), suggesting that ore-forming metals were derived from the mixture of Emeishan basalts and strata; ②Low Zn/Cd ratios (e.g. the Fule deposit), the deposits of this group have low Zn/Cd ratios (20-70), which are similar to that of sedimentary rocks, indicating that ore-forming metals were derived from the strata. Based on the Cd contents and Zn/Cd ratios, it's found that various ypes of Zn-Pb deposits have different Cd contents and Zn/Cd ratios. Therefore, the Cd content and the Zn/Cd ratio in sphalerite s are indicative in revealing the source of ore-forming materialsand genesis of Pb-Zn deposits.
-
Keywords:
- Zn/Cd ratios /
- sphalerite /
- Zn-Pb deposits /
- ore-forming metals /
- genesis of mineral deposit
-
-
高建京,毛景文,叶会寿,等.豫西沙沟脉状Ag-Pb-Zn 矿床地质特征和成矿流体研究[J].岩石学报,2010,26(3):740-756. GAO Jianjin,MAO Jingwen,YE Huisou, et al.Geology and ore-forming fluid of silver-lead-zinc lode deposit of Shagou,wester Henan Province[J].Acta Petrologic Sinica, 2010,26(3):740-756.
黄智龙,李文博,陈进,等.云南会泽超大型铅锌矿床C、O同位素地球化学[J].大地构造与成矿学, 2004, 1(28):53-59. HUANG Zhilong, LI Wenbo,CHEN Jin, et al.Carbon and Oxygen isotope geochmistry of the Huize superlarge Pb-Zn ore deposits in Yunnan Province[J].Geotectonica et Metallogenia, 2004, 1(28):53-59.
黄智龙,陈进,韩润生,等.云南会泽超大型铅锌矿床地球化学及成因-兼论峨眉山玄武岩与铅锌成矿的关系[M].北京:地质出版社, 2004:50-146. HUANG Zhilong,CHEN Jing,HAN Runsheng, et al. Geochmistry and Genesis of the Huize superlarge Pb-Zn ore deposits in Yunnan Province And the theory of emeishan basalt and lead-zinc metallogenic relationship[M].Beijing:Geological Publishing House, 2004:50-146.
江思宏,聂凤军,白大明,等.内蒙古白音诺尔铅锌矿床印支期成矿的年代学证据[J]. 矿床地质, 2011, 30(5):787-798. JIANG Sihong,NIE Fengjun,BAI Daming,et al. Geochronology evidence for Indosinian mineralization in Baiyinnuer Pb-Zn deposit of Inner Mongolia[J].Mineral Deposits, 2011, 30(5):787-798.
刘兵.阿尔金山喀腊达坂一带火山成因块状硫化物型铅锌矿床地质特征及找矿前景[J].西北地质,2014,47(4):264-268. LIU Bing. Geological Features and Ore Prospecting Potential of the Volcanogenic Massive Sulfide Lead-Zinc Deposits in Kaladaban Area,Altun[J].Northwestern Geology, 2014,47(4):264-268.
刘铁庚,叶霖,周家喜,等.闪锌矿的Fe、Cd关系随其颜色变化而变化[J].中国地质, 2010, 37(5):1457-1468. LIU Tiegeng, YE Lin, ZHOU Jiaxi, et al.The variation of Fe and Cd correlativity in sphalerite with the variation of the mineral color[J]. Geology in China, 2010, 37(5):1457-1468.
刘铁庚,裘愉卓,叶霖.闪锌矿颜色、成分和硫同位素之间的密切关系[J]. 矿物学报, 1994, 14(2):199-205. LIU Tiegeng,QIU Yuzhuo,YE Lin.Relationship between colour,chemical composition and sulfur isotopic composition of sphalerite[J].Acta Mineralogica Sinica, 1994, 14(2):199-205.
毛景文,郑榕芬,叶会寿,等.豫西熊耳山地区沙沟银铅锌矿床成矿的40Ar-39Ar 年龄及其地质意义[J].矿床地质, 2007, 25(4):359-368. MAO Jingwen,ZHENG Rongfen,YE Huishou, et al.40Ar/39Ar dating of fuchsite and sericite from altered rochs close to ore veins in Shagou large-size Ag-Pb-Zn deposit of Xiong ershan area, western Hennan Province,and its significance[J].Mineral Deposits, 2007, 25(4):359-368.
任鹏,梁婷,刘扩龙,等.秦岭凤太矿集区喷流沉积型铅锌矿床S、Pb同位素地球化学特征[J].西北地质,2014,47(1):137-149. REN Peng,LIANG Ting,LIU Kuolong,et al.Geochemistry of Sulfur and Lead Isotopic Compositions of Sedex Lead-zinc Deposits in Fengtai Mineral Cluster Region of Qinling Mountains[J]. Northwestern Geology, 2014,47(1):137-149.
涂光炽,高振敏,胡瑞忠,等.分散元素地球化学成矿机制[M].北京:地质出版社, 2004,1-153. TU Guangchi,GAO Zhenmin,HU Ruizhong,et al. Dispersed element geochemical metallogenic mechanism[M].Beijing:Geological Publishing House, 2004,1-153.
肖懿.呷村矿床的微量元素特征及其找矿方向[J].四川地质学报, 1993, 3(13):240-247. XIAO Yi.Trace element Geochemistry and prospecting target ofgacun argentiferous polymetallic ore depodit[J].Acta Geologica Sichuan, 1993, 3(13):240-247.
许典葵, 黄智龙, 邓红, 等.云南会泽超大型铅锌矿床的矿床模型[J]. 矿物学报, 2009, 29(2):235-242. XU Diankui, HUANG Zhilong,DENG Hong, et al.The deposit model of the world-class Huize Pb-Zn deposit,Yunnan Province,China[J].Acta Mineralogica Sinica, 2009, 29(2):235-242.
舒启海,赖勇,魏良民,等.大兴安岭南段白音诺尔铅锌矿床流体包裹体研究[J].岩石学报, 2011, 27(5):1467-1482. SHU Qihai,LAI Yong,WEI Liangmin, et al. Fluid inclusion study of the Baiyinnuo' er Zn-Pb deposit, south segment of the Great Xing' an Mountain, northeastern China[J].Acta Petrologica Sinica, 2011, 27(5):1467-1482.
谢华光,金庆民,蔡元吉.四川呷村多金属矿床地球化学特征及成因[J].火山地质与矿产, 1992, 2:37-47. XIE Huaguang,JIN Qingmin,CAI Yuanji.Gonesis and geochemical characteristics of gacun polymetallic deposit,sichuan[J].Volcanology Mineral Resources, 1992, 2:37-47.
叶庆同.四川呷村含金富银多金属矿床成矿地质特征和成因[J].矿床地质, 1991, 10(2):107-118. YE Qingtong.Geological characteristics and genesis of the gacun gold-bearing and silwer-rich polymetallic deposit, sichuan province[J].Mineral Deposits, 1991, 10(2):107-118.
叶会涛.华北陆块南缘中生代构造演化与铅锌银成矿作用[D].中国地质科学院博士论文. 北京:中国地质科学院,2006. YE Huitao. The southern margin of north China landmass Mesozoic tectonic evolution and lead-zinc mineralization of silver[D]. The Chinese academy of geological sciences doctoral dissertation.Beijing:Chinese Academy of Geological Sciences,2006. 张德全,鲍修文.内蒙古白音诺中酸性火山-深成杂岩体的岩石学,地球化学与成因研究[J].地质论评, 1990, 36(4):289-297. ZHANG Dequan,BAO Xiuwen.A study on the petrology,geochemistry and genesis of the Bayan Nur intermediate-acidic volcano-plutonic complex in eastem Inner Mongolia[J].Geological Review,1900, 36(4):289-297.
张振亮.云南会泽铅锌矿床成矿流体性质和来源-来自流体包裹体和水岩反应实验的证据[A].中国科学院研究生院博士论文[D].贵阳:中国科学院地球化学研究所,2006. ZHANG Zhenliang. Pb-Zn deposit metallogenic fluid properties and sources-from fluid inclusions and water-rock reaction experiment evidencet,Yunnan Province,China[A]. Graduate school of Chinese academy of sciences doctoral dissertation[D].Guiyang:Institute of geochemistry, Chinese Academy of Sciences,2006. 周家喜. 黔西北铅锌成矿区分散元素及锌同位素地球化学[A].中国科学院研究生院博士论文[D]. 贵阳:中国科学院地球化学研究所,2010. ZHOU Jiaxi. Qian lead-zinc metallogenic province northwest of dispersed elements and zinc isotope geochemistry[A]. Graduate school of Chinese academy of sciences doctoral dissertation[D].Guiyang:Institute of GeoChemistry, Chinese Academy of Sciences,2010. 朱传威, 温汉捷, 张羽旭, 等. 铅锌矿床中的 Cd 同位素组成特征及其成因意义[J]. 中国科学:地球科学, 2013, 11:014. ZHU Chuanwei,WEN Hanjie,ZHANG Yuxu,et al.Characteristics of Cd isotopic compositions and their genetic significance in the lead-zinc deposits of SW China[J].Science China:Earth Sciences, 2013, 11:014. BELISSONT R, BOIRON M C, LUAIS B, et al. LA-ICP-MS analyses of minor and trace elements and bulk Ge isotopes in zoned Ge-rich sphalerites from the Noailhac-Saint-Salvy deposit (France):Insights into incorporation mechanisms and ore deposition processes[J]. Geochimica et Cosmochimica Acta, 2014, 126:518-540.
COOK N J, CIOBANU C L, PRING A, et al. Trace and minor elements in sphalerite:A LA-ICPMS study[J]. Geochimica et Cosmochimica Acta, 2009, 73(16):4761-4791.
GOTTESMANN W, KAMPE A. Zn/Cd ratios in calcsilicate-hosted sphalerite ores at Tumurtijn-ovoo, Mongolia[J]. Chemie der Erde-Geochemistry, 2007, 67(4):323-328.
HAN R S, LIU C Q, HUANG Z L, et al. Geological features and origin of the Huize carbonate-hosted Zn-Pb-(Ag) district, Yunnan, South China[J]. Ore Geology Reviews, 2007, 31(1):360-383.
KHIN Z, STEPHEN G P, PAUL C, et al. Nature diversity of deposit types and metallogenic relations of South China[J]. Ore Geology Reviews, 2007, 31:3-47.
Mclimans R K, BARNES H L, OHMOTO H. Sphalerite stratigraphy of the upper Mississippi Valley zinc-lead district, southwest Wisconsin[J]. Economic Geology, 1980, 75(3):351-361.
METZ S, TREFRY J H. Chemical and mineralogical influences on concentrations of trace metals in hydrothermal fluids[J]. Geochimica et Cosmochimica Acta, 2000, 64(13):2267-2279.
ROEDDER E, DWORNIK E J. Sphalerite color banding lack of correlation with iron content, Pine Point, Northwest Territories, Canada[J]. American Mineralogist, 1968, 53:1523-1529.
SCHWARTZ M O. Cadmium in zinc deposits:Economic geology of a polluting element[J]. International Geology Review, 2000, 42:445-469.
WEN H J, ZHU C W, ZHANG Y X, et al. Zn/Cd ratios and cadmium isotope evidence for the classification of lead-zinc deposits[J]. Scientific Reports, 2016. DOI: 10.1038/srep25273.
XU Y, HUANG Z, ZHU D, et al. Origin of hydrothermal deposits related to the Emeishan magmatism[J]. Ore Geology Reviews, 2014, 63:1-8.
YE L, NIGEL J K, CRISTIANA L C, et al. Trace and minor elements in sphalerite from base metal deposits in South China:A LA-ICPMS study[J]. Ore Geology Reviews, 2011, 39:188-217.
YE L, COOK N J, CIOBANU C L, et al. Trace and minor elements in sphalerite from base metal deposits in South China:a LA-ICPMS study[J]. Ore Geology Reviews, 2011, 39(4):188-217.
ZENG Q D, LIU J M, ZHANG Z L, et al. Geology and Lead-Isotope Study of the Baiyinnuoer Zn-Pb-Ag Deposit, South Segment of the Da Hinggan Mountains, Northeastern China[J]. Resource Geology, 2009, 59(2):170-180.
ZHANG C, WU Y, HOU L, et al. Geodynamic setting of mineralization of Mississippi Valley-type deposits in world-class Sichuan-Yunnan-Guizhou Zn-Pb triangle, southwest China:Implications from age-dating studies in the past decade and the Sm-Nd age of Jinshachang deposit[J]. Journal of Asian Earth Sciences, 2015, 103:103-114.
计量
- 文章访问数: 2353
- HTML全文浏览量: 0
- PDF下载量: 2843