Re-Os Isotope Characteristics of the Huize Ultra-large Lead-Zinc Deposit, Northeastern Yunnan Province: Constraints on the Himalayan Metallogenic Dynamic Background

Xiao-jun JIANG; Zhong-qiang WANG; Chao LI; Zhong-lin GUO; Jian-hua CHAI; Wen-long QIU; Jia-sheng WANG

doi:10.15898/j.cnki.11-2131/td.201805030054

2018 Vol. 37, No. 4

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Article navigation > Rock and Mineral Analysis > 2018 > 37(4): 448-461

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Xiao-jun JIANG, Zhong-qiang WANG, Chao LI, Zhong-lin GUO, Jian-hua CHAI, Wen-long QIU, Jia-sheng WANG. Re-Os Isotope Characteristics of the Huize Ultra-large Lead-Zinc Deposit, Northeastern Yunnan Province: Constraints on the Himalayan Metallogenic Dynamic Background[J]. Rock and Mineral Analysis, 2018, 37(4): 448-461. doi: 10.15898/j.cnki.11-2131/td.201805030054

Citation:

Xiao-jun JIANG, Zhong-qiang WANG, Chao LI, Zhong-lin GUO, Jian-hua CHAI, Wen-long QIU, Jia-sheng WANG. Re-Os Isotope Characteristics of the Huize Ultra-large Lead-Zinc Deposit, Northeastern Yunnan Province: Constraints on the Himalayan Metallogenic Dynamic Background[J]. Rock and Mineral Analysis, 2018, 37(4): 448-461. doi: 10.15898/j.cnki.11-2131/td.201805030054

Re-Os Isotope Characteristics of the Huize Ultra-large Lead-Zinc Deposit, Northeastern Yunnan Province: Constraints on the Himalayan Metallogenic Dynamic Background

1.
Department of Earth Sciences, Kunming University of Science and Technology, Kunming 650093, China
2.
National Research Center for Geoanalysis, Beijing 100037, China
3.
Yunnan Chihong Zn & Ge Company LTD., Qujing 655000, China

More Information

Corresponding author: Chao LI, Re-Os@163.com

Received Date: 03 May 2018

Revised Date: 29 May 2018

Accepted Date: 11 June 2018

Abstract

Abstract

BACKGROUNDThe Huize ultra-large lead-zinc deposit is a typical MVT or HZT type deposit in the lead-zinc polymetallic belt. This deposit is known as a unique metallogenic system and germanium enrichment. Due to the low mineralization temperature and lack of suitable dating minerals, the age of the ore deposits has been controversial. OBJECTIVESTo precisely date the mineralization age by Negative Thermal Ionization Mass Spectrometry (NTIMS) Re-Os isotope analyses and discuss the Himalayan metallogenic dynamic process in the Huize ultra-large lead-zinc deposit. METHODSNTIMS Re-Os isotope analyses were carried out on pyrite, galena, and sphalerite samples collected from the Huize ultra-large lead-zinc deposit. The Re-Os isochron age from the pyrite, galena, and sphalerite samples was used to constrain mineralization age. The initial ¹⁸⁷Os/¹⁸⁸Os values were used to trace the material sources. RESULTSThe Re-Os isochron age of the pyrite samples is 40.7±2.6 Ma (2σ, n=9) with a model weighted average age of 40.0±2.6 Ma (2σ, n=8). The sphalerite and galena samples have model ages of 38.24±0.41 Ma and 36.57±0.40 Ma, respectively. Furthermore, the initial ¹⁸⁷Os/¹⁸⁸Os values of the pyrite samples vary from 0 to 0.26, whereas those of the sphalerite and galena samples are 0.46 and 0.41, respectively. CONCLUSIONSThe Re-Os isochron ages indicate that the mineralization for the Huize ultra-large lead-zinc deposit occurred during the Eocene period. Based on regional ore controlling structure, tectono-lithofacies alteration characteristics in Northeastern Yunnan and the isochron ages results, a two-stage (Yanshanian and Himalayan) tectonic-fluid metallogenic model for the Huize Ultra-large lead-zinc deposit is inferred.
- Northeastern Yunnan Province /
- Huize lead-zinc deposit /
- regional structural analysis /
- Re-Os isotope chronlogy

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References

[1]	谢家荣.云南矿产概论[J].地质论评, 1941(增刊):1-42. Google Scholar Xie J R.An introduction to the mineral resources in Yunnan Province[J].Geological Review, 1941(Supplement):1-42. Google Scholar
[2]	柳贺昌, 林文达.滇东北铅锌银矿床规律研究[M].昆明:云南大学出版社, 1999:1-419. Google Scholar Liu H C, Lin W D.Regularity Research of Ag-Zn-Pb Ore Deposits North-East Yunnan Province[M].Kunming:Yunnan University Press, 1999:1-419. Google Scholar
[3]	张长青. 中国川滇黔交界地区密西西比型(MVT)铅、锌矿床成矿模型[D]. 北京: 中国地质科学院, 2008. Google Scholar Zhang C Q. The Model of Mississippi Valley-type (MVT) Lead and Zinc Deposits in the Junction of Sichuan-Yunnan-Guizhou Provinces[D]. Beijing: Chinese Academy of Geological Sciences, 2008. Google Scholar
[4]	Zhou J X, Huang Z L, Bao G P.Geological and sulfur-lead-strontium isotopic studies of the Shaojiwan Pb-Zn deposit, Southwest China:Implications for the origin of hydrothermal fluids[J].Journal of Geochemical Exploration, 2013, 128(2):51-61. Google Scholar
[5]	Zhou J X, Huang Z L, Yan Z F.The origin of the Maozu carbonate-hosted Pb-Zn deposit, Southwest China:Constrained by C-O-S-Pb isotopic compositions and Sm-Nd isotopic age[J].Journal of Asian Earth Sciences, 2013, 73(5):39-47. Google Scholar
[6]	Zhou J X, Huang Z L, Zhou M F, et al.Constraints of C-O-S-Pb isotope compositions and Rb-Sr isotopic age on the origin of the Tianqiao carbonate-hosted Pb-Zn deposit, SW China[J].Ore Geology Reviews, 2013, 53(8):77-92. Google Scholar
[7]	王奖臻, 李朝阳, 李泽琴, 等.川滇地区密西西比河谷型铅锌矿床成矿地质背景及成因探讨[J].地质地球化学, 2001, 29(2):41-45. doi: 10.3969/j.issn.1672-9250.2001.02.007 CrossRef Google Scholar Wang J Z, Li Z Y, Li Z Q, et al.The geological setting, characters and origin of Mississippi valley-type Pb-Zn deposits in Sichuan and Yunnan provinces[J].Geology-Geochemistry, 2001, 29(2):41-45. doi: 10.3969/j.issn.1672-9250.2001.02.007 CrossRef Google Scholar
[8]	Zhou J X, Luo K, Wang X C, et al.Ore genesis of the fule Pb-Zn deposit and its relationship with the Emeishan large igneous province:Evidence from mineralogy, bulk C-O-S and in situ S-Pb isotopes[J].Gondwana Research, 2018, 54:161-179. doi: 10.1016/j.gr.2017.11.004 CrossRef Google Scholar
[9]	张长青, 毛景文, 刘峰, 等.云南会泽铅锌矿床粘土矿物K-Ar测年及其地质意义[J].矿床地质, 2005, 24(3):317-324. doi: 10.3969/j.issn.0258-7106.2005.03.011 CrossRef Google Scholar Zhang C Q, Mao J W, Liu F, et al.K-Ar dating of altered clay minerals from Huize Pb-Zn deposit in Yunnan Province and its geological significance[J].Mineral Deposits, 2005, 24(3):317-324. doi: 10.3969/j.issn.0258-7106.2005.03.011 CrossRef Google Scholar
[10]	毛景文, 周振华, 丰成友, 等.初论中国三叠纪大规模成矿作用及其动力学背景[J].中国地质, 2012, 39(6):1437-1471. doi: 10.3969/j.issn.1000-3657.2012.06.001 CrossRef Google Scholar Mao J W, Zhou Z H, Feng C Y, et al.A preliminary study of the Triassic large-scale mineralization in China and its geodynamic setting[J].Geology in China, 2012, 39(6):1437-1471. doi: 10.3969/j.issn.1000-3657.2012.06.001 CrossRef Google Scholar
[11]	韩润生, 王峰, 胡煜昭, 等.会泽型(HZT)富锗银铅锌矿床成矿构造动力学研究及年代学约束[J].大地构造与成矿学, 2014, 38(4):758-771. doi: 10.3969/j.issn.1001-1552.2014.04.003 CrossRef Google Scholar Han R S, Wang F, Hu Y Z, et al.Metallogenic tectonic dynamics and chronology constrains on the Huize-type (HZT) germanium-rich silver-lead-zinc deposits[J].Geotectonica et Metallogenia, 2014, 38(4):758-771. doi: 10.3969/j.issn.1001-1552.2014.04.003 CrossRef Google Scholar
[12]	芮宗瑶, 叶锦华, 张立生, 等.扬子克拉通周边及其隆起边缘的铅锌矿床[J].中国地质, 2004, 31(4):337-346. doi: 10.3969/j.issn.1000-3657.2004.04.001 CrossRef Google Scholar Rui Z Y, Ye J H, Zhang L S, et al.Pb-Zn deposits on the perimeter of the Yangtze craton and on the margins of its uplifts[J].Geology in China, 2004, 31(4):337-346. doi: 10.3969/j.issn.1000-3657.2004.04.001 CrossRef Google Scholar
[13]	黄智龙, 陈进, 刘丛强, 等.峨眉山玄武岩与铅锌矿床成矿关系初探——以云南会泽铅锌矿床为例[J].矿物学报, 2001, 21(4):681-688. doi: 10.3321/j.issn:1000-4734.2001.04.019 CrossRef Google Scholar Huang Z L, Chen J, Liu C Q, et al.A preliminary discussion on the genetic relationship between E'meishan basalts and Pb-Zn deposits as exemplified by the Huize Pb-Zn deposit, Yunnan Province[J].Acta Mineralogica Sinica, 2001, 21(4):681-688. doi: 10.3321/j.issn:1000-4734.2001.04.019 CrossRef Google Scholar
[14]	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[M].北京:地质出版社, 2004:1-300. Google Scholar Huang Z L, Chen J, Han R S, et.al.Genesis and Geochemistry of the Huize Superlarge Pb-Zn Ore Depositsin Yunnan Province[M].Beijing:Geological Publishing House, 2004:1-300. Google Scholar
[15]	李文博, 黄智龙, 王银喜, 等.会泽超大型铅锌矿田方解石Sm-Nd等时线年龄及其地质意义[J].地质论评, 2004, 50(2):189-195. doi: 10.3321/j.issn:0371-5736.2004.02.011 CrossRef Google Scholar Li W B, Huang Z L, Wang Y X, et al.Age of the giant Huize Zn-Pb deposits determined by Sm-Nd dating of hydrothermal calcite[J].Geological Review, 2004, 50(2):189-195. doi: 10.3321/j.issn:0371-5736.2004.02.011 CrossRef Google Scholar
[16]	蔺志永, 王登红, 张长青.四川宁南跑马铅锌矿床的成矿时代及其地质意义[J].中国地质, 2010, 37(2):488-494. doi: 10.3969/j.issn.1000-3657.2010.02.023 CrossRef Google Scholar Lin Z Y, Wang D H, Zhang C Q.Rb-Sr isotopic age of sphalerite from the Paoma lead-zinc deposit in Sichuan Province and its implications[J].Geology in China, 2010, 37(2):488-494. doi: 10.3969/j.issn.1000-3657.2010.02.023 CrossRef Google Scholar
[17]	鲍淼, 周家喜, 黄智龙, 等.铅锌矿床定年方法及川-滇-黔铅锌成矿域年代学研究进展[J].矿物学报, 2011, 31(3):391-396. Google Scholar Bao M, Zhou J X, Huang Z L, et al.Dating methods for Pb-Zn deposits and chronology research progress of Sichuan-Yunnan-Guizhou Pb-Zn metallogenic province:A review[J].Acta Mineralogica Sinica, 2011, 31(3):391-396. Google Scholar
[18]	吴越. 川滇黔地区MVT铅锌矿床大规模成矿作用的时代与机制[D]. 北京: 中国地质大学, 2013. Google Scholar Wu Y. The Age and Ore-forming Process of MVT Deposits in the Boundary Area of Sichuan-Yunnan-Guizhou provinces, Southwest China[D]. Beijing: China University of Geosciences, 2013. Google Scholar
[19]	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. doi: 10.3321/j.issn:0371-5736.2008.04.013 CrossRef Google Scholar Zhang C Q, Li X H, Yu J J, 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. doi: 10.3321/j.issn:0371-5736.2008.04.013 CrossRef Google Scholar
[20]	刘莹莹, 漆亮, 黄智龙, 等.滇东北富乐铅锌矿床硫化物Re-Os同位素年龄及其地质意义[J].矿物学报, 2013(增刊):599-600. Google Scholar Liu Y Y, Qi L, Huang Z L, et al.Re-Os isotopic age of sulphide from the Fule lead-zinc deposit in Northeastern Yunnan and its geological implications[J].Acta Mineralogica Sinica, 2013(Supplement):599-600. Google Scholar
[21]	周家喜. 黔西北铅锌成矿区分散元素及锌同位素地球化学[D]. 北京: 中国科学院大学, 2011. Google Scholar Zhou J X. Dispersing Elements and Zinc Isotopic Geochemistry for Pb-Zn Metallogenic Area in Northwest Guizhou Province[D]. Beijing: University of Chinese Academy of Sciences, 2011. Google Scholar
[22]	李文博, 黄智龙, 陈进, 等.云南会泽超大型铅锌矿床成矿物质来源:来自矿区外围地层及玄武岩成矿元素含量的证据[J].矿床地质, 2002, 21(增刊):413-416. Google Scholar Li W B, Huang Z L, Chen J, et al.Sources of ore-forming materials in Huize superlarge lead-zinc deposit, Yunnan Province:Evidence from contents of ore-forming element in strata and basalts from margin of ore district[J].Mineral Deposits, 2002, 21(Supplement):413-416. Google Scholar
[23]	张振亮. 云南会泽铅锌矿床成矿流体性质和来源[D]. 北京: 中国科学院研究生院(地球化学研究所), 2006. Google Scholar Zhang Z L. Properties and Sources of Ore-forming Fluids in Huize Pb-Zn Deposit, Yunnan Province[D]. Beijing: Graduate University Chinese Academy of Sciences (Institute of Geochemistry), 2006. Google Scholar
[24]	韩润生, 李波, 倪培, 等.闪锌矿流体包裹体显微红外测温及其矿床成因意义——以云南会超大型富锗银铅锌矿床为例[J].吉林大学学报(地球科学版), 2016, 46(1):91-104. Google Scholar Han R S, Li B, Ni P, et al.Infrared micro-thermometry of fluid inclusions in sphalerite and geological significance of Huize super-large Zn-Pb-(Ge-Ag) deposit, Yunnan Province[J].Journal of Jilin University (Earth Science Edition), 2016, 46(1):91-104. Google Scholar
[25]	任顺利, 李延河, 曾普胜, 等.膏盐层在云南会泽和毛坪铅锌矿成矿中的作用:硫同位素证据[J].地质学报, 2018, 92(5):1041-1055. doi: 10.3969/j.issn.0001-5717.2018.05.010 CrossRef Google Scholar Ren S L, Li Y H, Zeng P S, et al.Effect of sulfate evaporate salt layer in mineralization of the Huize and Maoping lead-zinc deposits in Yunnan:Evidence from sulfur isotope[J].Acta Geologica Sinca, 2018, 92(5):1041-1055. doi: 10.3969/j.issn.0001-5717.2018.05.010 CrossRef Google Scholar
[26]	陈进.麒麟厂铅锌硫化物矿床成因及成矿模式探讨[J].有色金属矿床与勘探, 1993, 2(2):90-99. Google Scholar Chen J.Genesis and metalogenic pattern of the Qilinchang Pb-Zn deposit[J].Geological Exploration for Non-Ferrous Metals, 1993, 2(2):90-99. Google Scholar
[27]	韩润生, 刘丛强, 黄智龙, 等.论云南会泽富铅锌矿床成矿模式[J].矿物学报, 2001, 21(4):674-680. doi: 10.3321/j.issn:1000-4734.2001.04.018 CrossRef Google Scholar Han R S, Liu C Q, Huang Z L, et al.Genesis modeling of Huize lead-zinc ore deposit in Yunnan[J].Acta Mineralogica Sinica, 2001, 21(4):674-680. doi: 10.3321/j.issn:1000-4734.2001.04.018 CrossRef Google Scholar
[28]	韩润生, 陈进, 李元, 等.云南会泽麒麟厂铅锌矿床构造地球化学及定位预测[J].矿物学报, 2001, 21(4):667-680. doi: 10.3321/j.issn:1000-4734.2001.04.017 CrossRef Google Scholar Han R S, Chen J, Li Y, et al.Tectono-geochemical features and orientation prognosis of concealed ores of Qilingchang lead-zinc deposit in Huize, Yunnan[J].Acta Mineralogica Sinica, 2001, 21(4):667-680. doi: 10.3321/j.issn:1000-4734.2001.04.017 CrossRef Google Scholar
[29]	韩润生, 陈进, 黄智龙, 等.构造成矿动力学及隐伏矿定位预测——以云南会泽铅锌(银、锗)矿床为例[M].北京:科学出版社, 2006:16-20, 85-95, 165-168. Google Scholar Han R S, Chen J, Huang Z L, et al.Dynamics of Tectonic Ore-forming Processes and Localization-Prognosis of Concealed Orebodies:As Exemplified by the Huize Super-large Zn-Pb-(Ag-Ge) District, Yunnan[M].Beijing:Science Press, 2006:16-20, 85-95, 165-168. Google Scholar
[30]	Zhou C X, Wei C S, Guo J Y, et al.The source of metals in the Qilinchang Zn-Pb deposit, Northeastern Yunnan, China:Pb-Sr isotope constraints[J].Economic Geology, 2001, 96(3):583-598. doi: 10.2113/gsecongeo.96.3.583 CrossRef Google Scholar
[31]	Brannon J C, Podosek F A, McLimans R K.Alleghenian age of the Upper Mississippi Valley lead-zinc deposit determined by Rb-Sr dating of sphalerite[J].Nature, 1992, 356:509-511. doi: 10.1038/356509a0 CrossRef Google Scholar
[32]	Brannon J C, Susan C C, Frank A, et al. Radiometric Dating of Ancient Calcite: Th-Pb & U-Pb Isochrones Fororest Age and Late-stage Calcite from the Central Tennessee Zinc District, An Appalachian-Ouachita Age MVT Deposit[C]. Abstracts with programs-Geological Society of America, 1995: 118. Google Scholar
[33]	Brannon J C, Susan C C, Frank A P, et al.Th-Pb and U-Pb dating of ore-stage calcite and Paleozoic fluid flow[J].Science, 1996, 271:491-493. doi: 10.1126/science.271.5248.491 CrossRef Google Scholar
[34]	Leach D L, Bradley D, Lewchuk M T, et al.Mississippi Valley-type lead-zinc deposits through geological time:Implications from recent age-dating research[J].Mineralium Deposita, 2001, 36(8):711-740. doi: 10.1007/s001260100208 CrossRef Google Scholar
[35]	Nakai S, Halliday A N, Kesler S E, et al.Rb-Sr dating of sphalerites from Tennessee and the genesis of Mississippi Valley type ore deposits[J].Nature, 1990, 346(6282):354-357. doi: 10.1038/346354a0 CrossRef Google Scholar
[36]	李超, 裴浩翔, 王登红, 等.山东孔辛头铜钼矿成矿时代及物质来源:来自黄铜矿、辉钼矿Re-Os同位素证据[J].地质学报, 2016, 90(2):240-249. doi: 10.3969/j.issn.0001-5717.2016.02.004 CrossRef Google Scholar Li C, Pei H X, Wang D H, et al.Age and source constraints for Kongxintou copper-molybdenum deposit Shandong from Re-Os isotope in molybdenite and chalcopyrite[J].Acta Geologica Sinica, 2016, 90(2):240-249. doi: 10.3969/j.issn.0001-5717.2016.02.004 CrossRef Google Scholar
[37]	杜安道, 屈文俊, 李超, 等.铼锇法及其在矿床学研究中的应用[M].北京:地质出版社, 2001. Google Scholar Du A D, Qu W J, Li C, et al.Re-Os Dating Method and Its Application to Ore Study[M].Beijing:Geological Publishing House, 2001. Google Scholar
[38]	屈文俊, 杜安道.高温密闭溶样电感耦合等离子体质谱准确测定辉钼矿铼-锇地质年龄[J].岩矿测试, 2003, 22(4):254-262. doi: 10.3969/j.issn.0254-5357.2003.04.003 CrossRef Google Scholar Qu W J, Du A D.The electrochemical behavior of dopamine on poly (cinchomeronic acid) modified glassy carbon electrode and its detection[J].Rock and Mineral Analysis, 2003, 22(4):254-262. doi: 10.3969/j.issn.0254-5357.2003.04.003 CrossRef Google Scholar
[39]	李超, 屈文俊, 周利敏, 等.Carius管直接蒸馏快速分离锇方法研究[J].岩矿测试, 2010, 29(1):14-16. doi: 10.3969/j.issn.0254-5357.2010.01.004 CrossRef Google Scholar Li C, Qu W J, Zhou L M, et al.Rapid separation of osmium by direct distillation with Carius tube[J].Rock and Mineral Analysis, 2010, 29(1):14-16. doi: 10.3969/j.issn.0254-5357.2010.01.004 CrossRef Google Scholar
[40]	周利敏, 高炳宇, 王礼兵, 等.Carius管直接蒸馏快速分离锇方法的改进[J].岩矿测试, 2012, 31(3):413-418. doi: 10.3969/j.issn.0254-5357.2012.03.005 CrossRef Google Scholar Zhou L M, Gao B Y, Wang L B, et al.Improvements on the separation method of osmium by direct distillation in Carius tube[J].Rock and Mineral Analysis, 2012, 31(3):413-418. doi: 10.3969/j.issn.0254-5357.2012.03.005 CrossRef Google Scholar
[41]	李超, 屈文俊, 杜安道, 等.铼-锇同位素定年法中丙酮萃取铼的系统研究[J].岩矿测试, 2009, 28(3):233-238. doi: 10.3969/j.issn.0254-5357.2009.03.008 CrossRef Google Scholar Li C, Qu W J, Du A D, et al.Comprehensive study on extraction of rhenium with acetone in Re-Os isotopic dating[J].Rock and Mineral Analysis, 2009, 28(3):233-238. doi: 10.3969/j.issn.0254-5357.2009.03.008 CrossRef Google Scholar
[42]	Creaser R A, Papanastassiou D A, Wasserburg G J.Negative thermal ion mass spectrometry of osmium, rhenium and iridium[J].Geochimica et Cosmochimica Acta, 1991, 55(1):397-401. doi: 10.1016/0016-7037(91)90427-7 CrossRef Google Scholar
[43]	Volkening J, Walczyk T, Heumann K G.Osmium isotope ratio determinations by negative thermal ion mass spectrometry[J].International Journal of Mass Spectrometry and Ion Processes, 1991, 105(2):147-159. doi: 10.1016/0168-1176(91)80077-Z CrossRef Google Scholar
[44]	Nier A O.A mass spectrometer for routine isotope abun-dance measurements[J].Review of Scientific Instruments, 1940, 11(7):212. doi: 10.1063/1.1751688 CrossRef Google Scholar
[45]	Smoliar M L, Walker R J, Morgan J W.Re-Os ages of group ⅡA, ⅡA, ⅣA and ⅣB iron meteorites[J].Science, 1996, 271:1099-1102. doi: 10.1126/science.271.5252.1099 CrossRef Google Scholar
[46]	Ludwig K.A Geochronogical Toolkit for Microsoft Excel(Version 2.0.)[M].Geochronology Center, 1999. Google Scholar
[47]	Liu Y, Hou Z Q, Tian S H, et al.Zircon U-Pb ages of the Mianning-Dechang syenites, Sichuan Province, Southwestern China:Constraints on the giant REE mineralization belt and its regional geological setting[J].Ore Geology Reviews, 2015, 64(8):554-568. Google Scholar
[48]	田世洪, 侯增谦, 袁忠信, 等.四川冕宁木落寨稀土矿床成岩成矿的⁴⁰Ar/³⁹Ar年代学研究[J].岩石学报, 2006, 22(10):2431-2436. Google Scholar Tian S H, Hou Z Q, Yuan Z X, et al.⁴⁰Ar/³⁹Ar geochro-nology of rocks and ores from the Muluozhai REE deposit in Mianning county, Sichuan Province[J].Acta Petrologica Sinica, 2006, 22(10):2431-2436. Google Scholar
[49]	Mao J W, Zhang Z C, Zhang Z H, et al.Re-Os isotopic dating of molybdenites in the Xiaoliugou W(Mo) deposit in the Northern Qilian Mountains and its geological significance[J].Geochimica et Cosmochimica Acta, 1999, 63(11-12):1815-1818. doi: 10.1016/S0016-7037(99)00165-9 CrossRef Google Scholar
[50]	Stein H J, Markey R J, Morgan J W, et al.The remark-able Re-Os chronometer in molybdenite:How and why it works[J].Terra Nova, 2001, 13(6):479-486. doi: 10.1046/j.1365-3121.2001.00395.x CrossRef Google Scholar
[51]	周柯, 叶会寿, 毛景文, 等.豫西鱼池岭斑岩型钼矿床地质特征及其辉钼矿铼-锇同位素年龄[J].矿床地质, 2009, 28(2):170-184. doi: 10.3969/j.issn.0258-7106.2009.02.006 CrossRef Google Scholar Zhou K, Ye H S, Mao J W, et al.Geological characteristics and molybdenite Re-Os isotopic dating of Yuchiling porphyry Mo deposit in Western Henan Province[J]. Mineral Deposits, 2009, 28(2):170-184. doi: 10.3969/j.issn.0258-7106.2009.02.006 CrossRef Google Scholar
[52]	Morelli R, Creaser R A, Seltmann R, et al.Age and source constraints for the giant Muruntau gold deposit, Uzbekistan, from coupled Re-Os-He isotopes in arsenopyrite[J].Geology, 2007, 35(9):795-798. doi: 10.1130/G23521A.1 CrossRef Google Scholar
[53]	张位及.试论滇东北铅锌矿床的沉积成因和成矿规律[J].地质与勘探, 1984(7):11-16. Google Scholar Zhang W J.Sedimentary origin and metallogenic regularity of Pb-Zn deposit in Northeastern Yunnan[J].Geology and Exploration, 1984(7):11-16. Google Scholar
[54]	廖文.滇东黔西铅锌金属区硫铅同位素组成特征与成矿模式探讨[J].地质与勘探, 1984(1):1-6. Google Scholar Liao W.Characteristics of sulfur and lead isotopic composition and metallogenic model for Pb-Zn metallogenic deposit, Eastern Yunnan and Western Guizhou Province[J].Geology and Exploration, 1984(1):1-6. Google Scholar
[55]	韩润生, 胡煜昭, 王学琨, 等.滇东北富锗银铅锌多金属矿集区矿床模型[J].地质学报, 2012, 86(2):280-294. Google Scholar Han R S, Hu Y Z, Wang X K, et al.Mineralization model of rich Ge-Ag-bearing Zn-Pb polymetallic deposit concentrated district in Northeastern Yunnan, China[J].Acta Geologica Sinica, 2012, 86(2):280-294. Google Scholar