[1]李玉成,赵书梅,贾立芹,等.邯郸娄里金矿铅同位素组成及其地质意义[J].西安科技大学学报,2017,(01):98-105.[doi:10.13800/j.cnki.xakjdxxb.2017.0116]
 LI Yu-cheng,ZHAO Shu-mei,JIA Li-qin,et al.Composition and implications of lead isotopic in Louli gold deposit,Handan district[J].Journal of Xi'an University of Science and Technology,2017,(01):98-105.[doi:10.13800/j.cnki.xakjdxxb.2017.0116]
点击复制

邯郸娄里金矿铅同位素组成及其地质意义(/HTML)
分享到:

西安科技大学学报[ISSN:1672-9315/CN:61-1434/N]

卷:
期数:
2017年01期
页码:
98-105
栏目:
出版日期:
2017-01-30

文章信息/Info

Title:
Composition and implications of lead isotopic in Louli gold deposit,Handan district
文章编号:
1672-9315(2017)01-0098-08
作者:
李玉成1赵书梅1贾立芹1王京涛1张良良1李随民2
1.河北省地矿局 第一地质大队,河北 邯郸 056000; 2.河北地质大学 资源学院,河北 石家庄 050031
Author(s):
LI Yu-cheng1ZHAO Shu-mei1JIA Li-qin1WANG Jing-tao1ZHANG Liang-liang1LI Sui-min2
1.The First Geological Team of Hebei Geological Exploration Bureau,Handan 056000,China; 2.College of Resources,Hebei GEO University,Shijiazhuang,050031,China
关键词:
金矿床 碱性岩体 娄里
Keywords:
Key words:gold deposit alkaline rock mass Louli
分类号:
TD 863
DOI:
10.13800/j.cnki.xakjdxxb.2017.0116
文献标志码:
A
摘要:
在邯郸永年洪山碱性杂岩体及其附近发现了数条金矿化带和多处铜矿化点。碱性杂岩体及其周边多金属及贵金属矿化的发现突破了以往邯郸-邢台地区只是矽卡岩式铁矿富集区的认识,找矿成果具有重要的理论和实践意义。以洪山碱性岩体北侧娄里金矿为例,测试分析了金矿石、斑岩体及不同围岩中Au,Cu等成矿元素含量,初步确定区内燕山期火成岩是形成金矿床和铜矿床重要的矿源层。在此基础上利用铅同位素示踪和分析了娄里金矿成矿物质来源,亦得出相同的结论。研究结果表明,形成碱性岩体的岩浆以地幔源为主,区内金、铜成矿元素均来源于幔源的碱性岩体。
Abstract:
Abstract:Several gold mineralization belts and copper mineralization points have been found in Hongshan alkaline complex rock mass and the adjacent area in Handan district.All these discoveries have brought a new conception that there is not only a place of skarn type iron ore enrichment region,but also is a potential prospecting area of nonferrous materials and precious metals.All this prospecting results have important theoretical and practical significance.Taking the Louli gold deposit as an example,which deposit located in the north of hongshan alkaline rock mass,we analyzed the metallogenic element and lead istotopic of ore,porphyry and different surrounding rock in order to find out the metallogenic material source.The analysis results have drawn a same conclusion that metallogenic material source mainly derived from the alkaline rock mass from which come gold and copper metallogenic.

参考文献/References:

[1] 赵振华,熊小林,王 强,等.我国富碱火成岩及有关的大型-超大型金铜矿床成矿作用[J].中国科学(D辑),2002,32(增刊):1-10. ZHAO Zhen-hua,XIONG Xiao-lin,WANG Qiang,et al.The mineralization of Large-super large copper Gold related to high alkaline igneous rocks in China[J].Science in China(Series D),2002,32(S):1-10. [2]李文光,王天刚,姚仲友,等.与碱性岩有关的浅成低温热液型金矿特征与控矿因素[J].地质通报,2014,33(2-3):308-317. LI Wen-guang,WANG Tian-gang,YAO Zhong-you,et al.Ore-controlling factors and exploration indicators of alkaline magmatism related epithermal gold deposits:A case study of the Porgera gold deposit in Papua New Guinea[J].Geological Bulletin of China,2014,33(2-3):308-317. [3]姚士新,吴良士,裴荣富.河北邯邢地区洪山岩体地质球化学及铜(金)矿化特征[J].地质与勘探,1993(5):11-16. YAO Shi-xin,WU Liang-shi,PEI Rong-fu.Geological,geochemical and mineralizational characteristics of Hongshan intrusive complex in Hand-Xingtai area,Hebei Province[J].Geology and Prospecting,1993(5):11-16. [4]徐桂林,石晓兰.河北武安地区冯昌金矿地质特征及成矿条件分析[J].地质调查与研究,2005,28(3):160-167. XU Gui-lin,SHI Xiao-lan.Geological characters of Fengchang gold deposit and its forming conditions in Wu'an,Hebei Province[J].Geological Survey and Research,2005,28(3):160-167. [5]徐桂林,石晓兰,许洪才.营里金矿地质特征及成矿条件分析[J].地质与勘探,2006,42(2):13-18. XU Gui-lin,SHI Xiao-lan,XU Hong-cai.Geological features and mineralization condition analysis of Yingli gold deposit[J].Geology and Prospecting,2006,42(2):13-18. [6]周 凌,陈 斌.南太行洪山正长岩体的成因和意义:锆石SHRIMP年代学、化学成分和Sr-Nd同位素特征[J].自然科学进展,2005,15(11):1 357-1 365. ZHOU Ling,CHEN Bin.The causes and significance of Hongshan syenite rock mass in South Taihang area:Zircon SHRIMP Geochronology,Chemical component and isotopic characteristics of Sr-Nd[J].Progress in Natural Science,2005,15(11):1 357-1 365. [7]迟清华,鄢明才.应用地球化学元素丰度数据手册[M].北京:地质出版,2007. CHI Qing-hua,YAN Ming-cai.Handbook of elemental abundance for applied geochemistry[M].Beijing:Geological Press,2007. [8]张 乾,潘家永,邵树勋.中国某些金属矿床矿石铅来源的铅同位素诠释[J].地球化学,2000,29(3):231-238. ZHANG Qian,PAN Jia-yong,SHAO Shu-xun.An interpretation of ore lead sourees from lead isotopic compositions of some ore dePosits in China[J].Geochimica,2000,29(3):231-238. [9]汪明启,高玉岩.利用铅同位素研究金属矿床地气物质来源:甘肃蛟龙掌铅锌矿床研究实例[J].地球化学,2007,36(4):391-399. WANG Ming-qi,GAO Yu-yan.Tracing source of geogas with lead isotopes:A case study in Jiaolongzhang Pb-Zn deposit,Gansu Province[J].Geochimica,2007,36(4):391-399. [10]吴开兴,胡瑞忠,毕献武,等.矿石铅同位素示踪成矿物质来源综述[J].地质地球化学,2002,30(3):73-81. WU Kai-xing,HU Rui-zhong,BI Xian-wu,et al.Ore lead isotopes as a tracer for ore-forming material sources:A review[J].Geochimica,2002,30(3):73-81. [11]邵铁全,刘云焕,席先武,等.新疆东天山典型金矿床成矿物质来源探讨[J].西安科技大学学报,2005,25(2):175-178. SHAO Tie-quan,LIU Yun-huan,XI Xian-wu,et al.Origin of minerogenetic substance for typical gold deposits in east Tianshan,Xinjiang[J].Journal of Xi'an University of Science and Technology,2005,25(2):175-178. [12]樊婷婷,周小虎,高 洁,等.东准噶尔红柳峡辉长岩锆石U-Pb年龄及地质意义[J].西安科技大学学报,2014,34(6):707-712. FAN Ting-ting,ZHOU Xiao-hu,GAO Jie,et al.U-Pb Zircon ages of the gabbro in Hongliuxia area of the eastern Junggar and its geological implications[J].Journal of Xi'an University of Science and Technology,2014,34(6):707-712. [13]梁 婷,王 磊,彭明兴,等.新疆彩霞山铅锌矿床的铅同位素地球化学研究[J].西安科技大学学报,2005,25(3):337-340. LIANG Ting,WANG Lei,PENG Ming-xing,et al.Characteristics of lead isotope for Caixia Mountain Pb-Zn deposit in Xinjiang[J].Journal of Xi'an University of Science and Technology,2005,25(3):337-340. [14]Doe B R,Zartman R E.Plumbotectonics 1.the Phanerozoic[C]//Barnes H L.Geochemistry of Hydrothermal Ore Deposits 2nd.Ed.Wilev Interscience,1979(2):22-70. [15]Zartman R E,Doe B R.Plumbotectonics the model[J].Tectonophys,1981,75:135-162. [16]Zartman R E,Haines S M.Thplumbotectonic model for Pb isotopic systematics among major terrestrial reservoirs:a case for bidirectional transport[J].Geochim.Cosmochim.Acta,1988,52:1 327-1 339. [17]陈 斌,翟明国,田 伟,等.太行山南段中生代杂岩体的岩石成因:元素和Nd-Sr-Pb同位素地球化学证据[J].矿物岩石地球化学通报,2005,24(2):93-102. CHEN Bin,ZHAI Ming-guo,TIAN Wei,et al.Petrogenesis of the mesozoic intrusive complexes from the Southern Taihang Orogen,North China Craton:Elemental and Sr-Nd-Pb isotopic constraints[J].Bulletin of Mineralogy,Petrology and Geochemistry,2005,24(2):93-102. [18]朱炳泉.矿石Pb同位素三维空间拓扑图解用于地球化学省与矿种区划[J].地球化学,1993(3):209-216. ZHU Bing-quan.Tri-dimension spacial topological diagrams of ore lead isotopes and their application to the division of geochemical provinces and mineralizations[J].Geochimica,1993(3):209-216. [19]朱炳泉.地球科学中同位素体系理论与应用——兼论中国大陆壳幔演化[M].北京:科学出版社,1998. ZHU Bing-quan.The theory and application of Isotope system in earth science:Crust-mantle evolution of mainland China[M].Beijing:Science Press,1998. [20]宋瑞先,魏明辉,何宇青,等.张家口地质矿产[M].北京:地质出版社,2013. SONG Rui-xian,WEI Ming-hui,HE Yu-qing,et al.Geology and mineral resources of Zhangjiakou area[M].Beijing:Geological Press,2013.

备注/Memo

备注/Memo:
基金项目:河北省国土资源厅基金(2012997039; 2014129497) 通讯作者:李玉成(1967-),男,辽宁建平人,高级工程师,E-mail:tswdlyc@163.com
更新日期/Last Update: 1900-01-01