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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第43卷

期数:

2021年第04期

页码:

661-643

栏目:

基础地质与矿产地质

出版日期:

2021-07-15

文章信息/Info

Title:

Rb-Sr Dating and Ore-forming Material Tracing of Sphalerite from Limei Pb-Zn Deposit in Huayuan Ore Concentration Area of Hunan, China

文章编号:

1672-6561(2021)04-0661-13

作者:

周 云; 段其发^*; 曹 亮; 于玉帅; 甘金木

(中国地质调查局武汉地质调查中心,湖北 武汉 430205)

Author(s):

ZHOU Yun;  DUAN Qi-fa^*;  CAO Liang;  YU Yu-shuai;  GAN Jin-mu

(Wuhan Center of China Geological Survey, Wuhan 430205, Hubei, China)

关键词:

Rb-Sr定年;  成矿时代;  铅锌矿床;  MVT型;  成矿物质;  花垣矿集区;  湖南;  扬子克拉通东南缘

Keywords:

Rb-Sr dating;  metallogenic epoch;  Pb-Zn deposit;  MVT;  ore-forming material;  Huayuan ore concentration area;  Hunan;  the southeastern margin of Yangtze craton

分类号:

P597; P611

DOI:

10.19814/j.jese.2020.08036

文献标志码:

A

摘要:

李梅铅锌矿床位于扬子克拉通东南缘花垣矿集区北段,预测铅锌储量为300×10⁴ t,是该区铅锌矿床的典型代表。该矿床铅锌矿体呈层状、似层状,受地层与构造的控制,主要赋存于下寒武统清虚洞组下段第三亚段地层藻灰岩中。为获得该矿床的成矿年龄,探讨其成矿物质来源,采用闪锌矿Rb-Sr定年方法,对主成矿期形成的闪锌矿单矿物进行Rb-Sr同位素组成测定,获得的等时线年龄为(464±12)Ma(平均标准权重偏差为0.97),成矿时代为中奥陶世,成矿早于花垣矿集区南段的狮子山铅锌矿床(成矿时间为(410±12)Ma)和柔先山铅锌矿床((412±6)Ma),推断在花垣矿集区范围内发生了郁南运动和广西运动导致的两期成矿事件,整个矿集区成矿时限跨度大约为70 Ma。李梅铅锌矿床成矿时代明显晚于赋矿地层时代,该矿床的形成可能与郁南运动形成伸展构造引起的构造热液活动有关。闪锌矿的⁸⁷Sr/⁸⁶Sr值为0.709 56～0.711 14,(⁸⁷Sr/⁸⁶Sr)_i值为0.709 380±0.000 018,成矿流体具有高于赋矿围岩的高Sr同位素比值,推断成矿物质应主要源自具有高⁸⁷Sr/⁸⁶Sr值和高Pb、Zn丰度的下伏寒武系石牌组和牛蹄塘组。

Abstract:

Limei Pb-Zn deposit is located in the northern part of Huayuan ore concentration area, the southeastern margin of Yangtze craton with a predicted reserve of 300×10⁴ t, which is the most typical Pb-Zn deposit in this area. The ore bodies in Limei Pb-Zn deposit are stratiform and stratoid, which are controlled by the strata and structures. They mainly occur in the algal limestone of the third sub-member of Lower Cambrian Qingxudong Formation. In order to obtain the metallogenic age of Limei Pb-Zn deposit and discuss the source of ore-forming materials, the isochron age of monomineral sphalerite formed in the main metallogenic period was yielded by Rb-Sr dating method. The obtained age is(464±12)Ma(MSWD is 0.97). The metallogenic epoch is Middle Ordovician, and the mineralization is earlier than that of Shizishan Pb-Zn deposit((410±12)Ma)and Rouxianshan Pb-Zn deposit((412±6)Ma)in the southern part of Huayuan ore concentration area. It is inferred that there are two metallogenic events in Huayuan ore concentration area caused by Yunan movement and Guangxi movement. The metallogenic time span of the whole ore concentration area is about 70 Ma. The mineralization age of Limei Pb-Zn deposit is obviously later than that of the host strata; the formation may be related to the tectonic hydrothermal activity caused by the extension structure during Yunan movement. The ⁸⁷Sr/⁸⁶Sr ratio of sphalerite ranges from 0.709 56 to 0.711 14, and the(⁸⁷Sr/⁸⁶Sr)_i is 0.709 380±0.000 018. The ore-forming fluid has a high Sr isotope ratio, which is higher than that of the host rock. It is inferred that the ore-forming materials should mainly come from the underlying Cambrian Shipai Formation and Niutitang Formation with high ⁸⁷Sr/⁸⁶Sr ratio and high abundances of Pb and Zn.

参考文献/References:

[1] 周 云,段其发,陈毓川,等.湘西花垣铅锌矿田成矿物质来源的C、O、H、S、Pb、Sr同位素制约[J].地质学报,2016,90(10):2786-2802. ZHOU Yun,DUAN Qi-fa,CHEN Yu-chuan,et al.C,O,H,S,Pb and Sr Isotope Constraints on the Metals Sources of Huayuan Pb-Zn Deposits in Western Hunan[J].Acta Geologica Sinica,2016,90(10):2786-2802. [2] 周 云.湘西花垣MVT型铅锌矿集区成矿作用研究[D].成都:成都理工大学,2017. ZHOU Yun.Metallogenesis Study of Huayuan MVT Type Pb-Zn Ore Concentration Area,Hunan[D].Chengdu:Chengdu University of Technology,2017. [3] WEI H T,XIAO K Y,SHAO Y J,et al.Modeling-based Mineral System Approach to Prospectivity Mapping of stratabound Hydrothermal Deposits:A Case Study of MVT Pb-Zn Deposits in the Huayuan Area,Northwestern Hunan Province,China[J].Ore Geology Reviews,2020,DOI:10.1016/j.oregeorev.2020.103368. [4] LI N,XIAO K Y,SUN L,et al.Part I:A Resource Estimation Based on Mineral System Modeling Prospectivity Approaches and Analogical Analysis:A Case Study of the MVT Pb-Zn Deposits in Huayuan District,China[J].Ore Geology Reviews,2018,101:966-984. [5] 段其发,曹 亮,曾健康,等.湘西花垣矿集区狮子山铅锌矿床闪锌矿Rb-Sr定年及地质意义[J].地球科学,2014,39(8):977-999. DUAN Qi-fa,CAO Liang,ZENG Jian-kang,et al.Rb-Sr Dating of Sphalerites from Shizishan Pb-Zn Deposit in Huayuan Ore Concentration Area,Western Hunan,and Its Geological Significance[J].Earth Science,2014,39(8):977-999. [6] 段其发.湘西—鄂西地区震旦系—寒武系层控铅锌矿成矿规律研究[D].武汉:中国地质大学,2014. DUAN Qi-fa.The Research of the Metallogenic Re-gularity of Stratabound Zinc-lead Deposits from Sinian-Cambrian in the Western Hunan and Eestern Hubei[D].Wuhan:China University of Geosciences,2014. [7] 李 堃,刘 飞,刘 凯,等.湘西—黔东地区铅锌矿床找矿模型与定量预测[J].吉林大学学报(地球科学版),2020,50(3):825-841. LI Kun,LIU Fei,LIU Kai,et al.Prospecting Model and Quantitative Prediction of Pb-Zn Deposits in Western Hunan and Eastern Guizhou[J].Journal of Jilin University(Earth Science Edition),2020,50(3):825-841. [8] 周 云,段其发,曹 亮,等.湘西花垣地区铅锌矿床流体包裹体显微测温与特征元素测定[J].地球科学,2018,43(7):2465-2483. ZHOU Yun,DUAN Qi-fa,CAO Liang,et al.Microthermometry and Characteristic Elements Determination of the Fluid Inclusions of the Huayuan Lead-zinc Deposit in Western Hunan[J].Earth Science,2018,43(7):2465-2483. [9] 周 云,段其发,唐菊兴,等.湘西花垣地区铅锌矿床C、H、O同位素特征及其对成矿流体来源的指示[J].地质通报,2017,36(5):823-833. ZHOU Yun,DUAN Qi-fa,TANG Ju-xing,et al.Carbon Hydrogen and Oxygen Isotopes of Huayuan Pb-Zn Ore Deposits in Western Hunan and Their Implications for the Source of Ore-forming Fluid[J].Geological Bulletin of China,2017,36(5):823-833. [10] 周 云,段其发,曹 亮,等.湘西花垣下寒武统清虚洞组灰岩与锶同位素研究[J].地层学杂志,2017,41(3):335-343. ZHOU Yun,DUAN Qi-fa,CAO Liang,et al.Strontium Isotope Compositions of the Lower Cambrian Qingxudong Formation and Pb-Zn Deposits in Huayuan,Western Hunan:Implications for Hydrothermal Mineralization[J].Journal of Stratigraphy,2017,41(3):335-343. [11] 谭娟娟,刘重芃,杨红梅,等.湘西花垣矿集区柔先山铅锌矿床的成矿时间和物质来源[J].地球科学,2018,43(7):2438-2448. TAN Juan-juan,LIU Chong-peng,YANG Hong-mei,et al.Geochronology and Ore-forming Material Source Constraints for Rouxianshan Pb-Zn Deposit in Huayuan Ore Concentration Area,Western Hunan[J].Earth Science,2018,43(7):2438-2448. [12] 曹 亮,段其发,彭三国,等.湘西地区铅锌矿成矿物质来源:来自S、Pb同位素的证据[J].地质通报,2017,36(5):834-845. CAO Liang,DUAN Qi-fa,PENG San-guo,et al.Sources of Metallogenic Materials of Lead-zinc Deposits in Western Hunan Province:Evidence from S and Pb Isotopes[J].Geological Bulletin of China,2017,36(5):834-845. [13] 周 云,段其发,唐菊兴,等.湘西地区铅锌矿的大范围低温流体成矿作用:流体包裹体研究[J].地质与勘探,2014,50(3):515-532. ZHOU Yun,DUAN Qi-fa,TANG Ju-xing,et al.The Large-scale Low-temperature Mineralization of Lead-zinc Deposits in Western Hunan:Evidence from Fluid Inclusions[J].Geology and Exploration,2014,50(3):515-532. [14] 刘文均,郑荣才.花垣铅锌矿床成矿流体特征及动态[J].矿床地质,2000,19(2):173-181. LIU Wen-jun,ZHENG Rong-cai.Characteristics and Movement of Ore-forming Fluids in the Huayuan Lead-zinc Deposit[J].Mineral Deposits,2000,19(2):173-181. [15] 杨绍祥,劳可通.湘西北铅锌矿床的地质特征及找矿标志[J].地质通报,2007,26(7):899-908. YANG Shao-xiang,LAO Ke-tong.Geological Characteristics and Ore Indicators of Lead-zinc Deposits in Northwestern Hunan,China[J].Geological Bulletin of China,2007,26(7):899-908. [16] 杨绍祥,劳可通.湘西北铅锌矿床碳氢氧同位素特征及成矿环境分析[J].矿床地质,2007,26(3):330-340. YANG Shao-xiang,LAO Ke-tong.A Tentative Discussion on Genesis of Lead-zinc Deposits in Northwest Hunan[J].Mineral Deposits,2007,26(3):330-340. [17] 匡文龙,刘新华,陈年生,等.湘西北下光荣矿区铅锌矿床主要地球化学特征[J].地质科学,2008,43(3):685-694. KUANG Wen-long,LIU Xin-hua,CHEN Nian-sheng,et al.Main Geochemical Characteristics of Lead-zinc Deposits in Xiaguangrong Ore District,Northwestern Hunan[J].Chinese Journal of Geology,2008,43(3):685-694. [18] 梁 薇,牟传龙,周恳恳,等.湘西花垣排碧寒武系花桥组上段—车夫组沉积环境的探讨[J].地质论评,2012,58(2):259-267. LIANG Wei,MOU Chuan-long,ZHOU Ken-ken,et al.A Discussion on Sedimentary Environment of the Upper Member of Huaqiao Formation-Chefu Formation of Cambrian in Paibi,Huayuan,Western Hunan[J].Geological Review,2012,58(2):259-267. [19] 汤朝阳,邓 峰,李 堃,等.湘西—黔东地区早寒武世沉积序列及铅锌成矿制约[J].大地构造与成矿学,2012,36(1):111-117. TANG Chao-yang,DENG Feng,LI Kun,et al.Sedimentary Sequence of the Lower Cambrian Qingxu-dong Formation in the Western Hunan and Eastern Guizhou Provinces and Its Constrains on Lead-zinc Mineralization[J].Geotectonica et Metallogenia,2012,36(1):111-117. [20] 蔡应雄,杨红梅,段瑞春,等.湘西—黔东下寒武统铅锌矿床流体包裹体和硫、铅、碳同位素地球化学特征[J].现代地质,2014,28(1):29-41. CAI Ying-xiong,YANG Hong-mei,DUAN Rui-chun,et al.Fluid Inclusions and S,Pb,C Isotope Geoche-mistry of Pb-Zn Deposits Hosted by Lower Cambrian in Western Hunan-eastern Guizhou Area[J].Geoscience,2014,28(1):29-41. [21] 李 堃,吴昌雄,汤朝阳,等.湘西黔东地区铅锌矿床C、O同位素地球化学特征及其对成矿过程的指示[J].中国地质,2014,41(5):1608-1619. LI Kun,WU Chang-xiong,TANG Chao-yang,et al.Carbon and Oxygen Isotopes of Pb-Zn Ore Deposits in Western Hunan and Eastern Guizhou Provinces and Their Implications for the Ore-forming Process[J].Geology in China,2014,41(5):1608-1619. [22] 毛党龙.湖南省花垣县大脑坡铅锌矿地质特征及成因[J].现代矿业,2016,32(2):90-94. MAO Dang-long.Geological Characteristics and Gene-sis of the Danaopo Pb-Zn Deposit in Huayuan County,Hunan Province[J].Modern Mining,2016,32(2):90-94. [23] 彭能立,刘 伟,梁恩云,等.湘西地区北洛塔和花垣铅锌矿田对比研究[J].地质找矿论丛,2016,31(2):190-198. PENG Neng-li,LIU Wei,LIANG En-yun,et al.A Comparative Study of Luota and Huayuan Lead-zinc Ore Field in the Northwest Hunan Province[J].Contributions to Geology and Mineral Resources Research,2016,31(2):190-198. [24] 赵佳进,许明珠,刘建平,等.湘西花垣铅锌矿田的成矿构造[J].地质找矿论丛,2016,31(3):346-354. ZHAO Jia-jin,XU Ming-zhu,LIU Jian-ping,et al.The Ore-forming Structural of Huayuan Lead-zinc Ore Field in Western Hunan Province[J].Contributions to Geology and Mineral Resources Research,2016,31(3):346-354. [25] 薛长军,吕古贤,高伟利,等.湘西花垣李梅矿田含矿层清虚洞期岩相古地理分析及成矿预测[J].地学前缘,2017,24(2):159-175. XUE Chang-jun,LU Gu-xian,GAO Wei-li,et al.Lithofacies Paleogeographic Analysis of Ore-bearing Layers in Qingxudong Period and Metallogenic Prediction in Limei Ore Field in Huayuan,Western Hunan,China[J].Earth Science Frontiers,2017,24(2):159-175. [26] 王 辰,刘建朝,张海东,等.湘西花垣地区奥陶—志留系沉积岩稀土元素地球化学特征及地质意义[J].矿物岩石地球化学通报,2017,36(3):516-522. WANG Chen,LIU Jian-chao,ZHANG Hai-dong,et al.REE Geochemical Characteristics of Ordovician-Silurian Sedimentary Rock in the Huayuan Area,Hunan Province and Their Geological Significances[J].Bulletin of Mineralogy,Petrology and Geochemistry,2017,36(3):516-522. [27] 夏新阶,舒见闻.李梅锌矿床地质特征及其成因[J].大地构造与成矿学,1995,19(3):197-204. XIA Xin-jie,SHU Jian-wen.Geologic Characteristics and Origin of the Limei Zinc Sulfide Deposit[J].Geotectonica et Metallogenia,1995,19(3):197-204. [28] 罗 卫,尹 展,孔 令,等.花垣李梅铅锌矿集区地质特征及矿床成因探讨[J].地质调查与研究,2009,33(3):194-202. LUO Wei,YIN Zhan,KONG Ling,et al.Discussion on the Geological Features and Genesis of the Limei Pb-Zn Ore Concentration Belt in North-western Hunan Province[J].Geological Survey and Research,2009,33(3):194-202. [29] 周 云,段其发,曹 亮,等.湖南花垣地区铅锌矿床稀土元素地球化学特征初步研究[J].华南地质与矿产,2017,33(3):282-292. ZHOU Yun,DUAN Qi-fa,CAO Liang,et al.A Preliminary Study on Rare Earth Elements Geochemical Characteristics of the Lead-zinc Deposits in Huayuan Area,Hunan Province[J]. Geology and Mineral Resources of South China,2017,33(3):282-292. [30] 陕 亮.湘东北地区铜-铅-锌-钴多金属成矿系统[D].北京:中国地质大学,2019. SHAN Liang.Metallogenic System of Copper-lead-zinc-cobalt Polymetallic Deposits,Northeastern Hu-nan Province,South China[D].Beijing:China University of Geosciences,2019. [31] MAXWELL R J.A Study of Rubidium,Strontium and Strontium Isotopes in Some Mafic and Sulfide Minerals[D].Vancouver:The University of British Columbia,1976. [32] 李文博,黄智龙,许德如,等.铅锌矿床Rb-Sr定年研究综述[J].大地构造与成矿学,2002,26(4):436-441. LI Wen-bo,HUANG Zhi-long,XU De-ru,et al.Rb-Sr Isotopic Method on Zinc-lead Ore Deposits:A Review[J].Geotectonica et Metallogenia,2002,26(4):436-441. [33] MEDFORD G A,MAXWELL R J,RICHARD L A.⁸⁷Sr/⁸⁶Sr Ratio Measurements on Sulfides,Carbonates and Fluid Inclusions from Pine Point,Northwest Territories,Canada:An ⁸⁷Sr/⁸⁶Sr Ratio Increase Accompanying the Mineralizing Process[J].Economic Geo-logy,1983,78(7):1375-1378. [34] NAKAI S,HALLIDAY A N,KESLER S E,et al.Rb-Sr Dating of Sphalerites from Tennessee and the Genesisi of Mississippi Valley Type Ore Deposits[J].Nature,1990,346:354-357. [35] BRANNON J C,PODOSEK F A,MCLIMANS R K.Alleghenian Age of the Upper Mississippi Valley Zinc-lead Deposit Determined by Rb-Sr Dating of Sphalerite[J].Nature,1992,356:509-511. [36] NAKAI S,HALLIDAY A N,KESLER S E,et al.Rb-Sr Dating of Sphalerites from Mississippi Valley-type(MVT)Ore Deposits[J].Geochimica et Cosmochimica Acta,1993,57(2):417-427. [37] CHRISTENSEN J N,HALLIDAY A N,LEIGH K E,et al.Direct Dating of Sulfides by Rb-Sr:A Critical Test Using the Polaris Mississippi Valley-type Zn-Pb Deposit[J].Geochimica et Cosmochimica Acta,1995,59(24):5191-5197. [38] CHRISTENSEN J N,HALLIDAY A N,VEARNCOMBE J R,et al.Testing Models of Large-scale Crustal Fluid Using Direct Dating of Sulfides:Rb-Sr Evidence Forearly Dewatering and Formation of Mississippi Valley-type Deposits,Canning Basin,Austra-lia[J].Economic Geology,1995,90(4):877-884. [39] 杨红梅,蔡 红,段瑞春,等.硫化物Rb-Sr同位素定年研究进展[J].地球科学进展,2012,27(4):379-385. YANG Hong-mei,CAI Hong,DUAN Rui-chun,et al.Progress in Rb-Sr Isotopic Dating of Sulfide[J].Advances in Earth Science,2012,27(4):379-385. [40] 李文博,黄智龙,陈 进,等.会泽超大型铅锌矿床成矿时代研究[J].矿物学报,2004,24(2):112-116. LI Wen-bo,HUANG Zhi-long,CHEN Jin,et al.Rb-Sr Dating of Mineral Assemblage from the Huize Giant Zn-Pb Deposit,Yunnan Provine[J].Acta Mineralogica Sinica,2004,24(2):112-116. [41] 喻 钢.辽东青城子矿田的年代学和同位素地球化学[D].合肥:中国科学技术大学,2005. YU Gang.The Chronology and Isotopic Geochemistry of Qingchengzi Ore Field,Eastern Liaoning[D].Hefei:University of Science and Technology of China,2005. [42] 张长青,李向辉,余金杰,等.四川大梁子铅锌矿床单颗粒闪锌矿铷-锶测年及地质意义[J].地质论评,2008,54(4):532-538. ZHANG Chang-qing,LI Xiang-hui,YU Jin-jie,et al.Rb-Sr Dating of Single Sphalerites from the Daliangzi Pb-Zn Deposit,Sichuan,and Its Geological Significances[J].Geological Review,2008,54(4):532-538. [43] 祁进平,宋要武,李双庆,等.河南省栾川县西沟铅锌银矿床单矿物铷-锶同位素组成特征[J].岩石学报,2009,25(11):2843-2854. QI Jin-ping,SONG Yao-wu,LI Shuang-qing,et al.Single-grain Rb-Sr Isotopic Composition of the Xigou Pb-Zn-Ag Deposit,Luanchuan,Henan Province[J].Acta Petrologica Sinica,2009,25(11):2843-2854. [44] 胡乔青,王义天,王瑞廷,等.陕西省凤太矿集区二里河铅锌矿床的成矿时代:来自闪锌矿Rb-Sr同位素年龄的证据[J].岩石学报,2012,28(1):258-266. HU Qiao-qing,WANG Yi-tian,WANG Rui-ting,et al.Ore-forming Time of the Erlihe Pb-Zn Deposit in the Fengxian-Taibai Ore Concentration Area,Shaanxi Province:Evidence from the Rb-Sr Isotopic Dating of Sphalerites[J].Acta Petrologica Sinica,2012,28(1):258-266. [45] 廖震文,王生伟,孙晓明,等.黔东北地区MVT型铅锌矿床闪锌矿Rb-Sr定年及其地质意义[J].矿床地质,2015,34(4):769-785. LIAO Zhen-wen,WANG Sheng-wei,SUN Xiao-ming,et al.Rb-Sr Dating of Sphalerites from MVT Pb-Zn Deposits in Northeastern Guizhou Province and Its Geological Implications[J].Mineral Deposits,2015,34(4):769-785. [46] 赵海杰,余长发,韩心巧,等.广东大降坪硫(铅锌)矿床岩浆热液叠加作用:来自闪锌矿Rb-Sr年龄及硫同位素的证据[J].矿床地质,2016,35(4):795-808. ZHAO Hai-jie,YU Zhang-fa,HAN Xin-qiao,et al.Magmatic Hydrothermal Superimposition in Dajiangping S(Pb-Zn)Deposit,Guangdong Province:Rb-Sr Isochron Age and Sulfur Isotope Evidence[J].Mineral Deposits,2016,35(4):795-808. [47] 于玉帅,刘阿睢,戴平云,等.贵州铜仁塘边铅锌矿床成矿时代和成矿物质来源:来自Rb-Sr同位素测年和S-Pb同位素的证据[J].地质通报,2017,36(5):885-892. YU Yu-shuai,LIU A-sui,DAI Ping-yun,et al.The Metallogenic Epoch and Ore-forming Material Source of the Tangbian Pb-Zn Deposit in Tongren,Guizhou Province:Evidence from Rb-Sr Dating of Sphalerites and S-Pb Isotope[J].Geological Bulletin of China,2017,36(5):885-892. [48] 王 健,张 均,张晓军,等.四川天宝山矿床闪锌矿Rb-Sr年代学、稳定同位素及地质意义[J].地球科学,2019,44(9):3026-3041. WANG Jian,ZHANG Jun,ZHANG Xiao-jun,et al.Rb-Sr Geochronology,Stable Isotopic Analyses and Geological Significance of the Tianbaoshan Pb-Zn Deposit in Sichuan Province,China[J].Earth Science,2019,44(9):3026-3041. [49] 刘军港,李子颖,聂江涛,等.相山铀矿田西部地区深部多金属矿化成矿年代与成矿流体演化:Rb-Sr同位素体系的制约[J].岩石学报,2019,35(9):2787-2800. LIU Jun-gang,LI Zi-ying,NIE Jiang-tao,et al.The Timing and Ore-forming Fluid Evolution of Deep Polymetalic Mineralization in Western Xiangshan Uranium Ore Field,South China:Constraints from Rb-Sr Isotope Systematics[J] Acta Petrologica Sinica,2019,35(9):2787-2800. [50] 侯鹤楠,任云生,陆思宇,等.吉林延边红太平铜多金属矿床脉型矿化的成矿时代与构造背景[J].岩石学报,2020,36(3):820-836. HOU He-nan,REN Yun-sheng,LU Si-yu,et al.Age and Tectonic Setting of Vein-type Mineralization of Hongtaiping Copper Polymetallic Deposit in Yanbian Area,Jilin Province,NE China[J].Acta Petrologica Sinica,2020,36(3):820-836. [51] 杨绍祥,余沛然,劳可通.湘西北地区铅锌矿床成矿规律及找矿方向[J].国土资源导刊,2006,3(3):92-98. YANG Shao-xiang,YU Pei-ran,LAO Ke-tong.Meta-llogenic Regularity and Prospecting Direction of Lead-zinc Deposits in Northwest Hunan[J].Land and Resources Herald,2006,3(3):92-98. [52] 李胜明.湘西北花垣铅锌矿田沉积-构造控矿机理及成矿远景预测[D].成都:成都理工大学,2016. LI Sheng-ming.Sedimentary Structure in Northwest Huayuan Lead-zinc Deposit in Hunan Metallogenic Mechanism and Metallogenic Prediction[D].Chengdu:Chengdu University of Technology,2016. [53] 胡太平,王敏芳,丁振举,等.湘西花垣李梅铅锌矿床C、O、S、Pb同位素特征及成矿物质来源[J].矿床地质,2017,36(3):623-642. HU Tai-ping,WANG Min-fang,DING Zhen-ju,et al.C,O,S and Pb Isotopic Characteristics and Sources of Metallogenic Materials of Limei Pb-Zn Deposit in Huayuan County,Western Hunan Province[J].Mine-ral Deposits,2017,36(3):623-642. [54] 杨红梅,刘重芃,段瑞春,等.贵州铜仁卜口场铅锌矿床Rb-Sr与Sm-Nd同位素年龄及其地质意义[J].大地构造与成矿学,2015,39(5):855-865. YANG Hong-mei,LIU Chong-peng,DUAN Rui-chun,et al.Rb-Sr and Sm-Nd Isochron Ages of Bokou-chang Pb-Zn Deposit in Tongren,Guizhou Province and Their Geological Implication[J].Geotectonica et Metallogenia,2015,39(5):855-865. [55] LUDWIG K R.User's Manual for Isoplot/Ex Rev.2.49:A Geochronological Toolkit for Microsoft Excel[R].Berkeley:Berkeley Geochronology Center,2001. [56] 路远发.GeoKit:一个用VBA构建的地球化学工具软件包[J].地球化学,2004,33(5):459-464. LU Yuan-fa.Geokit:A Geochemical Toolkit for Microsoft Excel[J].Geochimica,2004,33(5):459-464. [57] 舒良树.华南前泥盆纪构造演化:从华夏地块到加里东期造山带[J].高校地质学报,2006,12(4):418-431. SHU Liang-shu.Predevonian Tectonic Evolution of South China:from Cathaysian Block to Caledonian Period Folded Orogenic Belt[J].Geological Journal of China Universities,2006,12(4):418-431. [58] 周恳恳,许效松.扬子陆块西部古隆起演化及其对郁南运动的反映[J].地质论评,2016,62(5):1125-1133. ZHOU Ken-ken,XU Xiao-song.Evolution of Paleo-uplifts in the Western Upper Yangtze Craton and Its Reflection on Yunan Orogeny[J].Geological Review,2016,62(5):1125-1133. [59] 戴传固,陈建书,卢定彪,等.黔东南及邻区加里东运动的表现及地质意义[J].地质通报,2010,29(4):530-534. DAI Chuan-gu,CHEN Jian-shu,LU Ding-biao,et al.Appearance and Geologic Significance of Caledonian Movement in Southeastern Guizhou,China and Its Adjacent Area[J].Geological Bulletin of China,2010,29(4):530-534. [60] 周留煜.钦杭接合带西南段区域地质演化史和成矿效应[J].矿物学报,2011,31(增1):151-152. ZHOU Liu-yu.Regional Geological Evolution History and Metallogenic Effect of Southwest Qinhang Junction Zone[J].Acta Mineralogica Sinica,2011,31(S1):151-152. [61] 黄思静.上扬子地台区晚古生代海相碳酸盐岩的碳、锶同位素研究[J].地质学报,1997,71(1):45-53. HUANG Si-jing.A Study on Carbon and Strontium Isotopes of Late Paleozoic Carbonate Rocks in the Upper Yangtze Platform[J].Acta Geologica Sinica,1997,71(1):45-53. [62] 龚银杰,张遵遵,陈立波,等.川东南褶皱带洞岩铅锌矿床闪锌矿Rb-Sr同位素测年及其构造变形时代[J].中国地质,2020,47(2):485-496. GONG Yin-jie,ZHANG Zun-zun,CHEN Li-bo,et al.Sphalerite Rb-Sr Isotopic Dating of the Dongyan Pb-Zn Deposit in Southeastern Sichuan Fold Belt and Its Constraint on the Timing of Tectonic Deformation[J].Geology in China,2020,47(2):485-496. [63] DENISON R E,KIRKLAND D W,EVANS R.Using Strontium Isotopes to Determine the Age and Origin of Gypsum and Anhydrite Beds[J].The Journal of Geology,1998,106(1):1-18. [64] 曹 亮,梁玉明,段其发,等.扬子陆块东南缘升天坪锌矿床地质特征、闪锌矿Rb-Sr定年及其地质意义[J].高校地质学报,2018,24(4):504-515. CAO Liang,LIANG Yu-ming,DUAN Qi-fa,et al.Geological Characteristics and Rb-Sr Dating of Spha-lerites from the Shengtianping Zinc Deposit in Southeastern Yangtze Block and Its Geological Significance[J].Geological Journal of China Universities,2018,24(4):504-515.

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备注/Memo

备注/Memo:

收稿日期:2020-08-20; 修回日期:2020-10-12
基金项目:国家重点研发计划项目(2016YFC0600205); 中国地质调查局地质调查项目(DD20190811,DD20201152)
作者简介:周 云(1984-),女,安徽安庆人,助理研究员,理学博士,E-mail:zhouyun0910@163.com。
*通讯作者:段其发(1964-),男,云南腾冲人,教授级高级工程师,理学博士,E-mail:502xaohan@163.com。

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更新日期/Last Update: 2021-04-20